Cyamodus

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Cyamodus
Temporal range: Middle-Late Triassic,
247–235  Ma
Cyamodus 1.JPG
Fossil skeleton
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder:† Sauropterygia
Order:† Placodontia
Superfamily:† Cyamodontoidea
Family:† Cyamodontidae
Genus:† Cyamodus
Meyer, 1863
Species
  • †C. rostratus(Münster, 1839 [1] ) (type)
  • †C. hildegardisPeyer, 1931a
  • †C. kuhnschneyderiNosotti & Pinna 1993
  • †C. munsteri(Agassiz, 1833-45)
  • †C. orientalis(Wang et al., 2019) [1]
  • †C. tarnowitzensisGürich, 1884
Synonyms
  • Placodus rostratus, Muenster (1839)
  • Placodus muensteri, Aggassiz (1839)
  • Placodus laticeps, Meyer (1863)

Cyamodus (pron.: SIE-ah-MO-dus) is a genus of placodonts known from several species described from Middle-Late Triassic of Europe and China. The genus was described by Christian Erich Hermann von Meyer in 1863, based on specimens found in Germany. Like some other placodonts, Cyamodus has an armoured carapace composed of irregular hexagonal plates, with the mouth containing a small number of large, rounded teeth that were likely involved in crushing hard shelled organisms (durophagy).

Contents

Discovery

C. rostratus skull from below and above Cyamodus rostratus skull ventral and dorsal views.jpg
C. rostratus skull from below and above

Thus far, six species of Cyamodus have been identified - C. rostratus, C. munsteri, C. tarnowitzensis, C. hildegardis, C. kuhnschneyderi, [2] and C. orientalis.

Initially considered to be an ancestral turtle due to its testudine-like head and large, bifurcated carapace. However further investigation resulted in its reclassification as a placodont, and it is closely related to other turtle-like reptiles of the Triassic period such as Henodus and Psephoderma . [3] Similar to these other placodonts, Cyamodus lived hovering close to the sea floor, vacuuming up various shellfish, and crushing them between its blunt teeth. [4]

Historically, the first Cyamodus remains were found in Upper Muschelkalk shallow marine limestones at near Bayreuth in Bavaria (Germany). They included the incomplete holotype skulls of Cyamodus muensteri and Cyamodus rostatus, which along with all other placodont remains recovered from the six quarries on the Lainecker Range in northern Bavaria were originally considered to have been derived from fish. [5] The earliest Cyamodus skull was later restored by Muenster, with the addition of four teeth that had not been present in the original skull, and was named Placodus muensteri. [6]

Further placodont remains were found by Muenster, who collected many placodont cranial remains in the Bindlach and Lainecker Range quarries. All placodont remains from those sites were then revised as being of reptilian origin by Owen (1858). A complete Cyamodus skeleton, including its skull, is known for C. hildegardis, which was found outside the Germanic Basin in the northern Tethys in Switzerland. Middle Triassic sauropterygian placodonts have become increasingly important for developing new ideas to the evolutionary history of their relatives, the turtles, whereas modern analyses place placodonts not as their ancestors using morphological cladistic analyses based on the bone osteology. The study of these placodonts contributes to our understanding of the Germanic Basin and the reptile distributions. [6]

An intriguing placodont that appears to be intermediate between Cyamodus and the placochelyids, Protenodontosaurus italicus , was described by Giovanni Pinna in 1990. [4]

Description

Restoration of C. rostratus Cyamodus BW.jpg
Restoration of C. rostratus

Cyamodus was a relatively small reptile, with most species measuring 1.3–1.5 m (4.3–4.9 ft) long and weighing 20–25 kg (44–55 lb); the smallest species, C. rostratus, was about 0.9 m (3.0 ft) long and weighed 5 kg (11 lb). [1] [7] [8] [9] It was a heavily armored swimmer that fed mainly on shellfish that it was specialized to uproot and crush with its powerful jaws. [3] The body of Cyamodus, specifically the armor, has been described as possessing a turtle-like flatness. The shell was a two-part carapace on the upper surface of the body. The larger half covered Cyamodus from the neck to the hips and spread out flat, almost encompassing the limbs. The second, smaller plate covered the hips and the base of the tail. The shells themselves are covered in hexagonal or circular plates of armor. The skull is heart-shaped and broad. [2]

Distinct from Paraplacodus, the skull of Cyamodus had a shorter rostrum, a smaller orbit and a larger upper temporal fenestra that was rimmed by ossifications. The teeth were flat discs, only one tooth appeared on each premaxilla and only two teeth appeared on each maxilla, with the largest teeth on the pterygoid. The quadratojugal joined the squamosal and sealed up the lateral temporal fenestra from the ancestral species (Paraplacodus). [10]

The carapace of C. hildegardis has a series of similar-sized, enlarged lateral armor plates is rounder and less laterally expanded than was hypothesized. The separate pelvic shield, also carrying a smaller set of lateral armor plates that decrease in size with an anterior/posterior gradient covering mainly the pelvic girdle and the base of the tail. The short tail is armored by four series of armor plates that also show an anterior/posterior gradient of size reduction equivalent to the size reduction of the caudal vertebrae. [11] Until further fossils are recovered, the internal organisation of dermal plates within the two armor shields of C. hildegardis remains little known. [6]

Cyamodus did not have any dorsal spines, although it did have a wing-like elongated flattened lateral spine that served to brace the overlying subdermal carapace. Presumably, the dorsal spines disappeared to provide a closer and better braced association between the vertebrae and the carapace. [6]

Paleobiology

Underside of a C. hildegardis skull Cyamodus hildegardis.JPG
Underside of a C. hildegardis skull

Although the shell would most likely have been too cumbersome for highly adept swimming, Cyamodus would still have been more agile than other single shelled placodonts like Henodus. [12] The shells were also covered in hexagonal plates that not only increased the level of protection but also increased their weight, a typical placodont adaptation as additional weight just beyond the level of neutral buoyancy allowed them to dive to reach shellfish. Other adaptations for protection besides the heavily armored shell include the strongly built rear of the skull and limbs that do not protrude too far. Although the reduction in limb length restricted its ability to swim, its heavy shell greatly assisted its ability to dive. Cyamodus is also expected to have had difficulty maneuvering on land and probably only ventured out of the water for periods of rest. Discovery of two fossil Cyamodus juveniles inside the stomach area of a Lariosaurus fossil has led to speculation about its vulnerability to predation. [13] [14]

It has also been noted that juvenile specimens of Cyamodus have an extra tooth on the roof of their mouth, compared to adult specimens. This suggests that Cyamodus reduced the number of teeth as they grew to maturity. However, this could be due to a difference between species of Cyamodus. [4]

Underside of a C. kuhnschnyderi skull Cyamodus kuhnschnyderi.JPG
Underside of a C. kuhnschnyderi skull

C. hildegardis from the Besano Formation (Middle Triassic) of the Alpine area of Switzerland and northern Italy has been reconstructed with a broad, laterally expanded main armor (carapace) and a separate smaller pelvic shield, giving it a sprawling appearance. [11] A reexamination of the postcranial dermal armor and endoskeletal elements of the three best preserved articulated specimens of the species has led to new interpretations of the dermal armor and underlying postcranial bones, as well as a new life reconstruction. [6] [11]

Placodus and Cyamodus Placodus and Cyamodus.jpg
Placodus and Cyamodus

Placodonts are typically considered to be durophagous (adapted to crushing hard-shelled organisms). [15] C.G. Diedrich has suggested that Cyamodus and other placodonts were algae-grazers. [6] However, this interpretation has been criticized by Torsten M. Scheyer and other researchers, [15] and many subsequent studies about placodonts have rejected Deidrich's interpretation, and the consensus that placodonts with the exception of Henodus were durophagous still continues to be strongly supported. [16] [17] [18] [19] [20] [21]

Related Research Articles

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Sauropterygia is an extinct taxon of diverse, aquatic reptiles that developed from terrestrial ancestors soon after the end-Permian extinction and flourished during the Triassic before all except for the Plesiosauria became extinct at the end of that period. The plesiosaurs would continue to diversify until the end of the Mesozoic. Sauropterygians are united by a radical adaptation of their pectoral girdle, adapted to support powerful flipper strokes. Some later sauropterygians, such as the pliosaurs, developed a similar mechanism in their pelvis. It is possible that sauropterygians are a distant relatives of turtles, uniting them under the group Pantestudines, although this is still debatable as sauropterygians might be archosauromorphs or completely unrelated to both.

<i>Placodus</i> Extinct genus of reptiles

Placodus is an extinct genus of marine reptiles belonging to the order Placodontia, which swam in the shallow seas of the middle Triassic period. Fossils of Placodus have been found in Central Europe and China.

<span class="mw-page-title-main">Placodontia</span> Extinct order of Triassic marine reptiles

Placodonts are an extinct order of marine reptiles that lived during the Triassic period, becoming extinct at the end of the period. They were part of Sauropterygia, the group that includes plesiosaurs. Placodonts were generally between 1 and 2 m in length, with some of the largest measuring 3 m (9.8 ft) long.

<span class="mw-page-title-main">Euryapsida</span>

Euryapsida is a polyphyletic group of sauropsids that are distinguished by a single temporal fenestra, an opening behind the orbit, under which the post-orbital and squamosal bones articulate. They are different from Synapsida, which also have a single opening behind the orbit, by the placement of the fenestra. In synapsids, this opening is below the articulation of the post-orbital and squamosal bones. It is now commonly believed that euryapsids are in fact diapsids that lost the lower temporal fenestra. Euryapsids are usually considered entirely extinct, although turtles might be part of the sauropterygian clade while other authors disagree. Euryapsida may also be a synonym of Sauropterygia sensu lato.

<i>Placochelys</i> Extinct genus of reptiles

Placochelys is an extinct genus of placodont reptiles erected by Otto Jaekel in 1902.

<span class="mw-page-title-main">Thalattosauria</span> Extinct group of marine reptiles

Thalattosauria is an extinct order of marine reptiles that lived in the Middle to Late Triassic. Thalattosaurs were diverse in size and shape, and are divided into two superfamilies: Askeptosauroidea and Thalattosauroidea. Askeptosauroids were endemic to the Tethys Ocean, their fossils have been found in Europe and China, and they were likely semiaquatic fish eaters with straight snouts and decent terrestrial abilities. Thalattosauroids were more specialized for aquatic life and most had unusual downturned snouts and crushing dentition. Thalattosauroids lived along the coasts of both Panthalassa and the Tethys Ocean, and were most diverse in China and western North America. The largest species of thalattosaurs grew to over 4 meters (13 feet) in length, including a long, flattened tail utilized in underwater propulsion. Although thalattosaurs bore a superficial resemblance to lizards, their exact relationships are unresolved. They are widely accepted as diapsids, but experts have variously placed them on the reptile family tree among Lepidosauromorpha, Archosauromorpha, ichthyosaurs, and/or other marine reptiles.

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References

  1. 1 2 3 Wei Wang; Chun Li; Torsten M. Scheyer; Lijun Zhao (2019). "A new species of Cyamodus (Placodontia, Sauropterygia) from the early Late Triassic of south-west China". Journal of Systematic Palaeontology. 17 (17): 1237–1256. doi:10.1080/14772019.2018.1535455. S2CID   91579582.
  2. 1 2 Dixon, Dougal (2006). The Complete Book of Dinosaurs . Hermes House.
  3. 1 2 Strauss, Bob. "Cyamodus". About. Archived from the original on 2015-09-06. Retrieved 2015-03-06.
  4. 1 2 3 Naish, Darren. "Placodonts: The Bizarre 'Walrus-Turtles' of the Triassic". Indiana University.
  5. ↑ Callaway, Jack; et al. (1997). Ancient Marine Reptiles . Academic Press. pp.  138–140. ISBN   978-0080527215.
  6. 1 2 3 4 5 6 Diedrich, Cajus G. (2011). "The shallow marine placodont Cyamodus of the central European Germanic Basin: its evolution, paleobiogeography and paleoecology". Historical Biology: An International Journal of Paleobiology. 24.3 (4): 1–19. doi:10.1080/08912963.2011.575938. S2CID   128569569.
  7. ↑ Furrer, H. (2004). "Der Monte San Giorgio im Südtessin – vom Berg der Saurier zur Fossil-Lagerstätte internationaler Bedeutung" (PDF). Neujahrsblatt herausgegeben von der Naturforschenden Gesellschaft in Zürich: 18. S2CID   127398058.
  8. ↑ Paul, Gregory S. (2022). The Princeton Field Guide to Mesozoic Sea Reptiles. Princeton University Press. pp. 77–79. doi:10.1515/9780691241456. ISBN   9780691193809. S2CID   251553177.
  9. ↑ Diedrich, C.G. (2012). "The Middle Triassic marine reptile biodiversity in the Germanic Basin,in the centre of the Pangaean world". Central European Journal of Geosciences. 4 (1): 9–46. doi: 10.2478/s13533-011-0060-0 . S2CID   129930258.
  10. ↑ Jiang, Da-Yong; et al. (2008). "First Record of Placodontoidea (Reptilia, Sauropterygia, Placodontia) from the Eastern Tethys" (PDF). Journal of Vertebrate Paleontology. 28 (3): 904–908. doi:10.1671/0272-4634(2008)28[904:froprs]2.0.co;2. S2CID   9784064. Archived from the original (PDF) on 2015-04-02.
  11. 1 2 3 Owen, R. (1858). "Description of the skull and teeth of the Placodus laticeps, Owen, with indications of other new species of Placodus, and evidence of the saurian nature of that genus". Philosophical Transactions of the Royal Society of London. 148: 169–184. doi: 10.1098/rstl.1858.0009 . S2CID   111331431.
  12. ↑ Westphal, F. (1976). "The dermal armour of some Triassic placodont reptiles". Linnean Society Symposium Series Academic Press, London. 3: 34–41.
  13. ↑ Rieppel, O.; et al. (1999). A skull of Cyamodus kuhnschnyderi Nosotti & Pinna 1993, from the Muschelkalk of Wassonne. France: Paläontologische Zeitschrift. pp. 377–383.
  14. ↑ Renesto, S.; et al. (1995). "Functional Morphology and Mode of Life of the Late Triassic placodont Psephoderma alpinum Meyer from the Calcare di Zorino (Lombardy, N Italy)". Rivista Italiana di Paleontologia e Stratigrafia. 101 (1): 37–48.
  15. 1 2 Scheyer, Torsten M.; Neenan, James M.; Renesto, Silvio; Saller, Franco; Hagdorn, Hans; Furrer, Heinz; Rieppel, Olivier; Tintori, Andrea (2012-06-01). "Revised paleoecology of placodonts – with a comment on 'The shallow marine placodont Cyamodus of the central European Germanic Basin: its evolution, paleobiogeography and paleoecology' by C.G. Diedrich (Historical Biology, iFirst article, 2011, 1–19, doi: 10.1080/08912963.2011.575938)". Historical Biology. 24 (3): 257–267. doi:10.1080/08912963.2011.621083. ISSN   0891-2963. S2CID   83707481.
  16. ↑ Crofts, Stephanie B.; Neenan, James M.; Scheyer, Torsten M.; Summers, Adam P. (2017). "Tooth occlusal morphology in the durophagous marine reptiles, Placodontia (Reptilia: Sauropterygia)". Paleobiology. 43 (1): 114–128. doi:10.1017/pab.2016.27. ISSN   0094-8373. S2CID   88556195.
  17. ↑ Klein, Nicole; Houssaye, Alexandra; Neenan, James M.; Scheyer, Torsten M. (2015-02-23). "Long bone histology and microanatomy of Placodontia (Diapsida: Sauropterygia)". Contributions to Zoology. 84 (1): 59–S15. doi: 10.1163/18759866-08401005 . ISSN   1875-9866.
  18. ↑ Neenan, James M; Li, Chun; Rieppel, Olivier; Bernardini, Federico; Tuniz, Claudio; Muscio, Giuseppe; Scheyer, Torsten M (2014). "Unique method of tooth replacement in durophagous placodont marine reptiles, with new data on the dentition of Chinese taxa". Journal of Anatomy. 224 (5): 603–613. doi:10.1111/joa.12162. ISSN   0021-8782. PMC   3981503 . PMID   24517163.
  19. ↑ Neenan, James M.; Klein, Nicole; Scheyer, Torsten M. (2013-03-27). "European origin of placodont marine reptiles and the evolution of crushing dentition in Placodontia". Nature Communications. 4 (1): 1621. Bibcode:2013NatCo...4.1621N. doi: 10.1038/ncomms2633 . ISSN   2041-1723. PMID   23535642. S2CID   21274778.
  20. ↑ Klein, Nicole; Scheyer, Torsten M. (2014). "A new placodont sauropterygian from the Middle Triassic of the Netherlands". Acta Palaeontologica Polonica. 59 (4): 887–902. doi: 10.4202/app.2012.0147 .
  21. ↑ Pommery, Yannick; Scheyer, Torsten M.; Neenan, James M.; Reich, Tobias; Fernandez, Vincent; Voeten, Dennis F. A. E.; Losko, Adrian S.; Werneburg, Ingmar (2021-07-05). "Dentition and feeding in Placodontia: tooth replacement in Henodus chelyops". BMC Ecology and Evolution. 21 (1): 136. doi: 10.1186/s12862-021-01835-4 . ISSN   2730-7182. PMC   8256584 . PMID   34225664.
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