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Cyclotosaurus

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Cyclotosaurus
Temporal range: Middle Triassic–Late Triassic
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Order: †Temnospondyli
Suborder: †Stereospondyli
Clade: †Capitosauria
Family: †Mastodonsauridae
Genus: †Cyclotosaurus
Fraas, 1889
Type species
†Cyclotosaurus robustus
(Meyer & Plienninger, 1844)
Other species
  • †C. mordax Fraas, 1913
  • †C. posthumus Fraas, 1913
  • †C. ebrachensis Kuhn, 1932
  • †C. hemprichi Kuhn, 1942
  • †C. intermedius Sulej & Majer, 2005
  • †C. buechneri Witzmann, Sachs & Nyhuis, 2016
  • †C.? papilio Wepfer [de], 1923
  • †C. naraserluki Marzola et al., 2017
Synonyms

Cyclotosaurus is an extinct genus of temnospondyl within the family Mastodonsauridae. It was of great size for an amphibian, had an elongated skull up to 56 cm (22 in).[1][2]

Etymology

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The name means "round eared lizard" in Ancient Greek, derived from round openings or fenestrae in the cheeks, which are thought to contain structures of the middle ear.[3]

History

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Cyclotosaurus mordax skull

German naturalist Eberhard Fraas erected the genus Cyclotosaurus in 1889, with C. robustus (previously Mastodonsaurus robustus) as the type species.[4] Several species are known, mainly from Germany and Poland in Central Europe, as well as East Greenland and Thailand.[5][6] The relationships between species is unclear.[1]

"Labyrinthodon" pachygnathus Owen, 1842 and "L." leptognathus Owen, 1842 were transferred to Cyclotosaurus, as C. pachygnathus and C. leptognathus, by Paton (1974).[7] However, Damiani (2001) assigned the two species to Mastodonsauroidea indeterminate and Stereospondyli indeterminate.[4]

Palaeontology

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Cyclotosaurus intermedius model

The genus is known from the Ladinian in the Middle Triassic to the Norian in the Late Triassic, and represents the last of the Mastodonsaurids.[4]

Life restoration of Cyclotosaurus

The oldest, questionable, species is Cyclotosaurus papilio, known from a partial skull recovered from the Ladinian (Middle Triassic) age Upper Muschelkalk beds from Baden-Württemberg in Germany.[4] Cyclotosaurus robustus is known from the Carnian (Late Triassic) Schilfsandstein Formation in Stuttgart-Feuerbach in Germany, while C. ebrachensis has been described from the Blasensandstein Formation in Ebrach.[8] Cyclotosaurus intermedius has been described from lacustrine deposits dated to the late Carnian in Krasiejów in southern Poland. It is so named as it has features intermediate between the more ancient C. robustus and more recent C. mordax. Importantly, postcranial material of this species has been recovered, which is unusual this genus.[1] Cyclotosaurus hemprichi is known from the Norian (Late Triassic) age Knollenmergel of Halberstadt, and Cyclotosaurus posthumus from the Stubensandstein (Norian) in Pfaffenhofen.[8] A partial skull very similar to C. posthumus has been recovered from the Norian (Late Triassic) Huai Hin Lat Formation near Chulabhorn Dam in Northeastern Thailand.[6] In 2016 a new species, C. buechneri, was described from the Late Triassic (middle Carnian) Stuttgart Formation of Bielefeld, the northernmost record in Germany.[9] In 2017, Cyclotosaurus naraserluki, a new endemic species from the Fleming Fjord Fm., East Greenland, was described as the closest Cyclotosaurus species to C. mordax, also being the westernmost and northernmost known species of Cyclotosaurus.[2] In 2019 a Cyclotosaurus humerus was reported from a Rhaetian aged bone bed within Bonenburg clay pit in eastern North Rhine-Westphalia, Germany. This represents the only definitive non-brachyopoid Rhaetian temnospondyl, and the last known record of Capitosauria.[10]

Phylogeny

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The phylogeny of Capitosauroidea according to Witzmann et al. (2016).[9]

Capitosauroidea

The phylogeny of the genus Cyclotosaurus according to Witzmann et al. (2016).[9]

Cyclotosaurus

C. robustus

C. buechneri

C. mordax

C. ebrachensis

C. intermedius

C. posthumus

C. hemprichi

See also alternative phylogenies from 2017[2] with the description of C. naraserluki.

Ecology

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Cyclotosaurus are thought to have been semi-aquatic carnivores, though feeding strategies likely differed between species.[1]

References

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  1. ^ a b c d Sulej, T.; Majer, D. (2005). "The temnospondyl amphibian Cyclotosaurus from the Upper Triassic of Poland" (PDF). Palaeontology. 48: 157–70. doi:10.1111/j.1475-4983.2004.00430.x.
  2. ^ a b c Marzola, M., Mateus O., Shubin N. H., & Clemmensen L. B. (2017). Cyclotosaurus naraserluki, sp. nov., a new Late Triassic cyclotosaurid (Amphibia, Temnospondyli) from the Fleming Fjord Formation of the Jameson Land Basin (East Greenland). Journal of Vertebrate Paleontology. e1303501., 2017
  3. ^ Schoch, Rainer (2008). "The Capitosauria (Amphibia): characters, phylogeny, and stratigraphy" (PDF). Palaeodiversity. 1: 189–226.
  4. ^ a b c d Damiani, Ross J. (2001). "A systematic revision and phylogenetic analysis of Triassic mastodonsauroids (Temnospondyli: Stereospondyli)". Zoological Journal of the Linnean Society. 133 (4): 379–482. doi:10.1111/j.1096-3642.2001.tb00635.x.
  5. ^ Jenkins, F. A. Jr.; Shubin, N. H.; Amaral, W. W.; Gatesy, S. M.; Schaff, C. R.; Clemmensen, L. B.; Downs, W. R.; Davidson, A. R.; Bonde, N.; Osbaeck, F. (1994). "Late Triassic continental vertebrates and depositional environments of the Fleming Fjord Formation, Jameson Land, East Greenland". Meddelelser om Grønland, Geoscience. 32: 1–25.
  6. ^ a b Ingavat, Rucha; Janvier, Phillippe (1981). "Cyclotosaurus cf. Posthumus Fraas (Capitosauridae, Stereospondyli) from the Huai Hin Lat Formation (Upper Triassic), Northeastern Thailand". Geobios. 14 (6): 711–25. doi:10.1016/S0016-6995(81)80149-0.
  7. ^ PATON, R. L. 1974. Capitosauroid labyrinthodonts from the Trias of England. Palaeontology, 17, 253–289, pls 35–36.
  8. ^ a b Nicholas C. Fraser; Hans-Dieter Sues (1997). In the Shadow of the Dinosaurs: Early Mesozoic Tetrapods. Cambridge University Press. p. 8. ISBN 0521458994.
  9. ^ a b c Witzmann, F.; Sachs, S.; Nyhuis, C.J. (2016). "A new species of Cyclotosaurus (Stereospondyli, Capitosauria) from the Late Triassic of Bielefeld, NW Germany, and the intrarelationships of the genus" (PDF). Fossil Record. 19 (2): 83–100. doi:10.5194/fr-19-83-2016.
  10. ^ Konietzko-Meier, Dorota; Werner, Jennifer D.; Wintrich, Tanja; Martin Sander, P. (June 2019). "A large temnospondyl humerus from the Rhaetian (Late Triassic) of Bonenburg (Westphalia, Germany) and its implications for temnospondyl extinction". Journal of Iberian Geology. 45 (2): 287–300. doi:10.1007/s41513-018-0092-0. ISSN 1698-6180. S2CID 134049099.
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