Biology:Udanoceratops
| Udanoceratops | |
|---|---|
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| Skeletal reconstruction | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Dinosauria |
| Clade: | †Ornithischia |
| Suborder: | †Ceratopsia |
| Family: | †Leptoceratopsidae |
| Genus: | †Udanoceratops Kurzanov, 1992 |
| Species: | †U. tschizhovi
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| Binomial name | |
| †Udanoceratops tschizhovi Kurzanov, 1992
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Udanoceratops (meaning "Udan's horned face") is a genus of large leptoceratopsid dinosaur that lived during the Late Cretaceous period of Mongolia, in what is now the Djadokhta Formation.
Discovery
Udanoceratops was first named and described by Russia n paleontologist Sergei Kurzanov in 1992 and the type species is Udanoceratops tschizhovi. The holotype (PIN 3907/11) was collected during the 1980s at the Udan Sayr (also spelled Udyn Sayr or Üüden Sair) locality of the Djadokhta Formation in Ömnögovi Province, dating to the Campanian stage of the Late Cretaceous period. The generic name is derived from the name of the locality in which the holotype was found (Udan Sayr) and Greek ceras/κέρας meaning "horn" and -ops/ωψ meaning "face". Udanoceratops is best known from the holotype specimen, which represents a large individual comprising a large, relatively well-preserved and almost complete skull, and sparse body remains including vertebrae.[1]
In 1993 a large skull ("nearly 1 m long") assigned to Udanoceratops was reported from the nearby Bayan Mandahu Formation by paleontologist Tomasz Jerzykiewicz.[2] However, Polish paleontologist Łukasz Czepiński in 2020 pointed out that there are no referable specimens to Udanoceratops from the Bayan Mandahu collections, and it is most likely that these remains were confused with the concurring (and relatively large) Protoceratops hellenikorhinus.[3]
In 2004 Viktor S. Tereschhenko referred a juvenile specimen (PIN 4046/11) to Udanoceratops aff. tschizhovi, from the Baga Tariach locality in Dornogovi Province, which Tereschhenko attributed to the Djadokhta Formation.[4] Geological analyses carried out across fossiliferous localities of the Gobi Desert published by Mahito Watabe and team in 2010, indicates that this locality instead correlates best with the Maastrichtian-stage Barun Goyot Formation.[5] The assignment of this specimen, however, has varied since then from "Udanoceratops" sp.,[6][7] to ?Udanoceratops sp.[8]
Description
Udanoceratops was a large ceratopsian, estimated at to have reached nearly 4 m (13 ft) long with a weight of 700 kg (1,500 lb).[9] It is the largest leptoceratopsid known so far.[10] The skull had a short frill and no horns over the eyes or nose. Its skull was about 60 cm (600 mm) long. The lower jaw was distinctively robust.[1]
Classification
Udanoceratops belonged to the Ceratopsia (the name is derived Greek meaning 'horned face'), a group of herbivorous dinosaurs with parrot-like beaks which thrived in North America and Asia during the Cretaceous Period.[1] It is placed within the Leptoceratopsidae, as the only Asian representative at the time, along with the North American Leptoceratops, Montanoceratops and Prenoceratops.[10]
Paleobiology
Udanoceratops, like all ceratopsians, was a herbivore. The short, deep jaws would have given the animal a powerful bite. The toothless beak would have served to grasp and crop stems or leaves, and as in other leptoceratopsids, the teeth would have met with an action that combined shearing and crushing. The feeding adaptations seen in leptoceratopsids suggest a diet of relatively tough food items, however little is known about the plants that grew in the Gobi Desert during the Cretaceous.[10]
See also
References
- ↑ 1.0 1.1 1.2 Kurzanov, S. M. (1992). "Новый род протоцератопсид из позднего мела Монголии" (in ru). Paleontological Journal: 81−93.
- ↑ Jerzykiewicz, T.; Currie, P. J.; Eberth, D. A.; Johnston, P. A.; Koster, E. H.; Zheng, J.-J. (1993). "Djadokhta Formation correlative strata in Chinese Inner Mongolia: an overview of the stratigraphy, sedimentary geology, and paleontology and comparisons with the type locality in the pre-Altai Gobi". Canadian Journal of Earth Sciences 30 (10): 2180−2195. doi:10.1139/e93-190. Bibcode: 1993CaJES..30.2180J. https://www.researchgate.net/publication/237174446.
- ↑ Czepiński, Ł. (2020). "New protoceratopsid specimens improve the age correlation of the Upper Cretaceous Gobi Desert strata". Acta Palaeontologica Polonica 65 (3): 481−497. doi:10.4202/app.00701.2019. http://www.app.pan.pl/archive/published/app65/app007012019.pdf.
- ↑ Tereschhenko, V. S. (2004). "О гетероцельных позвонках у рогатых динозавров (Protoceratopidae, Neoceratopsia)". Paleontological Journal (2): 81−86.
- ↑ Watabe, M.; Tsogtbaatar, K.; Suzuki, S.; Saneyoshi, M. (2010). "Geology of dinosaur fossil bearing localities (Jurassic and Cretaceous: Mesozoic) in the Gobi Desert: Results of the HMNS-MPC Joint Paleontological Expedition". Hayashibara Museum of Natural Sciences Research Bulletin 3: 41–118. https://www.academia.edu/3119116.
- ↑ Tereschenko, V. S. (2007). "Key to Protoceratopoid Vertebrae (Ceratopsia, Dinosauria) from Mongolia". Paleontological Journal 41 (2): 175−188. doi:10.1134/S0031030107020086. https://www.researchgate.net/publication/226106749.
- ↑ Tereschhenko, V. S. (2008). "Adaptive Features of Protoceratopsids (Ornithischia: Neoceratopsia)". Paleontological Journal 42 (3): 50−64. doi:10.1134/S003103010803009X. https://www.researchgate.net/publication/226432157.
- ↑ Kuznetsov, A. N.; Tereschenko, V. S. (2015). "Methods for Size Reconstruction in Distorted and Damaged Vertebrae of Fossil Tetrapods". Paleontological Journal 49 (3): 293−303. doi:10.1134/S0031030115030120. https://www.researchgate.net/publication/292476236.
- ↑ Paul, G. S. (2016). The Princeton Field Guide to Dinosaurs (2nd ed.). Princeton, New Jersey: Princeton University Press. pp. 278. ISBN 9780691167664.
- ↑ 10.0 10.1 10.2 Dodson, P. (1996). The Horned Dinosaurs. Princeton University Press, Princeton, New Jersey. ISBN 0-691-05900-4. https://archive.org/details/horneddinosaursn00dods_0.
External links
Wikidata ☰ Q132581 entry
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