| Sinotyrannus Temporal range:
Early Cretaceous,
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|---|---|
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| Skeletal diagram of Sinotyrannus based on Yutyrannus and other proceratosaurids | |
Scientific classification
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Dinosauria |
| Clade: | Saurischia |
| Clade: | Theropoda |
| Family: | † Proceratosauridae |
| Genus: | †
Sinotyrannus Ji et al., 2009 |
| Type species | |
|
†Sinotyrannus kazuoensis Ji et al., 2009
| |
Sinotyrannus (meaning “Chinese tyrant”) was a early, large-bodied genus within the superfamily Tyrannosauroidea [1]. This dinosaur had a single type species, S. kazuoensis, with the only known specimen containing a partial skull, some vertebrae, and a hip [2], all of which were found in the Early Cretaceous aged Jiufotang Formation of Liaoning, China. While it exhibited greater body size that would put it on par with the later tyrannosaurids such as Tyrannosaurus (a group that Sinotyrannus was initially suspected of being in), Sinotyrannus was probably a member of the basal tyrannosaur family known as the Proceratosauridae. This family originated in the Jurassic, whose members are known from Europe and Asia. Sinotyrannus, alongside another early tyrannosaur, Yutyrannus, appears to have been oddly large when compared to most tyrannosaurs of the Early Cretaceous, such as Dilong. Most of the world during the Early Cretaceous was dominated by more basal tetanurans, such as the megalosaurs and allosaurs, with tyrannosaurids themselves only taking over after both groups started to decline. However, Sinotyrannus and Yutyrannus appear to be exceptions to this. Sinotyrannus was the largest theropod in the Jiufotang Formation, reaching up to 10 meters (32.8 ft) in overall length and having a general mass similar to that of a large rhino. [3]
This animal was quite likely an active predator, as has been speculated for most tyrannosaurs, and may have been covered in a simple feathery coat as was the case with most basal coelurosaurs, including many early tyrannosaurs [4]. Sinotyrannus lived in a rather wet environment with well-watered forests and large lakes. The area experienced great diversity in terms of vertebrate fauna, with many taxa, such as Microraptor, living alongside Sinotyrannus. Despite this, the area was quite prone to high volcanism [5]. S. kazuoensis, was described by Ji et al. in 2009. [2]
Description
Sinotyrannus was a large tyrannosaur, measuring approximately 9–10 metres (30–33 ft) long and weighing 2.5 metric tons (2.8 short tons). [2] [6] It was among the largest basal tyrannosauroids known, repudiating the previously presumed trend that tyrannosauroids gradually increased in size throughout the Cretaceous period from small basal forms like Dilong to advanced apex predators such as Tyrannosaurus. The holotype, KZV-001, consists of a disarticulated partial skeleton including the front portion of the skull, three dorsal vertebrae, incomplete ilia, three articulated manual phalanges (including an ungual), and other fragmentary bones. [2]
The described cranial elements include the premaxillae, dentary, and anterior portions of the maxillae and nasals. The dorsal margin of the maxilla is unusually concave unlike the convex condition in tyrannosaurids. The nares are large and elliptical, supporting its relation to proceratosauridae. The dentary gradually curves upwards as it approaches its front edge. Many teeth are preserved attached to the maxillae, with a roughly equal number of denticles on each side, similarly to those of tyrannosaurids. Sinotyrannus could perceivably have had a tall nasal crest like other proceratosaurids, although not enough of its nasals are preserved to be certain. [2] [7]
The three preserved vertebrae have very tall neural spines. The proportions of the preserved manual phalanges support the idea that they belong to the second finger, and the ungual has a deep groove on each side. The ilia are mainly present as molds, with the mold of the external side of the left ilium being the most complete. The preacetabular blade is short and wide, with a massive pubic peduncle, while the postacetabular blade is longer and thinner, with a triangular ischial peduncle. These traits of the ilia differentiate it from more advanced tyrannosauroids such as the tyrannosaurids. [2]
Classification
The original description of Sinotyrannus proposed that it could have been the earliest tyrannosaurid due to its large size, [2] but subsequent analyses place it as a proceratosaurid tyrannosauroid. A 2013 study by Loewen et al. considered it to be part of a clade containing Juratyrant and Stokesosaurus, as they all reputedly share a narrow preacetabular notch. The results of their phylogenetic analyses are shown in the cladogram below: [7]
However, Brusatte et al. (2016) instead placed Juratyrant and Stokesosaurus outside of the Proceratosauridae, and proposed that Sinotyrannus represents the sister taxon of Yutyrannus within proceratosauridae. The results of their phylogenetic analyses are shown in the cladogram below: [8]
| Proceratosauridae | |
See also
References
- ^ Brusatte, S. L.; Norell, M. A.; Carr, T. D.; et al. (2010). "Tyrannosaur paleobiology: new research on ancient exemplar organisms" (PDF). Science. 329 (5998): 1481–1485. Bibcode: 2010Sci...329.1481B. doi: 10.1126/science.1193304. hdl: 20.500.11820/fc52fb23-10e8-466d-a7e9-081260d166c6. PMID 20847260. S2CID 45978858.
- ^ a b c d e f g Ji, Q.; Ji, S.-A.; Zhang, L.-J. (2009). "First large tyrannosauroid theropod from the Early Cretaceous Jehol Biota in northeastern China" (PDF). Geological Bulletin of China. 28 (10): 1369–1374. Archived from the original (PDF) on 1 October 2018.
- ^ Holtz, Thomas R.; Rey, Luis V. (2007). Dinosaurs: the most complete, up-to-date encyclopedia for dinosaur lovers of all ages (PDF) (Supplementary material) (1 ed.). New York: Random House. ISBN 978-0-375-82419-7.
- ^ Xu, Xing; Norell, Mark A.; Kuang, Xuewen; Wang, Xiaolin; Zhao, Qi; Jia, Chengkai (October 2004). "Basal tyrannosauroids from China and evidence for protofeathers in tyrannosauroids". Nature. 431 (7009): 680–684. doi: 10.1038/nature02855. ISSN 0028-0836.
- ^ Qin, Zuohuan; Xi, Dangpeng; Wagreich, Michael; Sames, Benjamin; Tong, Xiaoning; Hu, Jianfang; Yu, Zhiqiang; Wan, Xiaoqiao (2021-08-01). "Living environment of the early Jehol Biota: A case study from the Lower Cretaceous Dabeigou Formation, Luanping Basin (North China)". Cretaceous Research. 124: 104833. doi: 10.1016/j.cretres.2021.104833. ISSN 0195-6671.
- ^ Paul, Gregory S. (2010). The Princeton Field Guide to Dinosaurs. New Jersey: Princeton University Press. pp. 99. ISBN 9780691137209.
- ^ a b Loewen, M.A.; Irmis, R.B.; Sertich, J.J.W.; Currie, P. J.; Sampson, S. D. (2013). Evans, David C (ed.). "Tyrant Dinosaur Evolution Tracks the Rise and Fall of Late Cretaceous Oceans". PLoS ONE. 8 (11): e79420. Bibcode: 2013PLoSO...879420L. doi: 10.1371/journal.pone.0079420. PMC 3819173. PMID 24223179.
- ^ Brusatte, Stephen L.; Carr, Thomas D. (2016-02-02). "The phylogeny and evolutionary history of tyrannosauroid dinosaurs". Scientific Reports. 6 (1): 20252. Bibcode: 2016NatSR...620252B. doi: 10.1038/srep20252. ISSN 2045-2322. PMC 4735739. PMID 26830019.
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