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Asiatyrannus
Genus of tyrannosaurid dinosaurs From Wikipedia, the free encyclopedia
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Asiatyrannus (meaning "Asian tyrant") is an extinct genus of tyrannosaurine theropod dinosaurs from the Late Cretaceous Nanxiong Formation of China. The genus contains a single species, A. xui, known from a single specimen consisting of a skull and partial postcranial skeleton. Asiatyrannus is notable for its deep-snouted skull and small body size, in contrast to the gracile snout and larger size of the contemporary Qianzhousaurus. It represents the southernmost record of an Asian tyrannosaurid.[2]
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Discovery and naming
The Asiatyrannus holotype specimen, ZMNH M30360, was discovered in September 2017 in sediments of the Nanxiong Formation near Shahe Town in Nankang District of Ganzhou City, Jiangxi Province, China. The specimen consists of most of an articulated skull in addition to disarticulated parts of the postcrania, comprising much of the right and left legs and several caudal vertebrae.[2]
In 2024, Zheng et al. described Asiatyrannus xui as a new genus and species of tyrannosaurid based on these fossil remains. The generic name, Asiatyrannus, combines "Asia", the continent of origin, with the Latinised Greek suffix "-tyrannus", meaning "tyrant" or "king". The specific name, xui, honors prominent dinosaur researcher Xu Xing and his contributions to paleontological research in China.[2]
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Description
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Asiatyrannus is a small-medium-sized tyrannosaur. Its nearly complete skull measures 47.5 centimetres (18.7 in) long, and it has an estimated body length of 3.5–4 metres (11–13 ft).[2] In comparison, the mature skull of the closely related Nanuqsaurus from the Prince Creek Formation of North America is estimated at 60–70 centimetres (24–28 in).[3] Since Nanuqsaurus likely had a body size similar to Albertosaurus, Asiatyrannus may represent the only tyrannosaurine in this smaller size class.[4] The Asiatyrannus holotype is about half the length of the contemporary Qianzhousaurus. However, the holotype of Asiatyrannus with the estimated age of at least 13 years old did not belong to a skeletally mature individual, and as such, it would have been larger when fully grown. Nevertheless, it had probably passed through the life stages of most rapid growth, and other tyrannosaurines in similar growth stages are more than twice as large.[2]
In their 2025 description of the early-diverging tyrannosauroid Khankhuuluu, Voris and colleagues noted several problematic aspects of the original interpretations of the Asiatyrannus holotype. The researchers claimed that the histology performed and lines of arrested growth (LAGs) identified by Zheng and colleagues the year prior did not support the specimen as having passed the rapid-growth phase, meaning it can not be regarded as mature. Voris et al. further noted six traits initially regarded as diagnostic to Asiatyrannus that it shares with Tarbosaurus specimens or other tyrannosaurines (three of which are present only in immature specimens).[5]
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Classification
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Using a modified version of the phylogenetic dataset of Carr et al. (2017),[6] Zheng et al. recovered Asiatyrannus as a derived tyrannosaurine member of the Tyrannosauridae, in a polytomy with the North American Nanuqsaurus. These results are displayed in the cladogram below:[2]
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Voris et al. (2025) reidentified Asiatyrannus as a juvenile tyrannosaurine sharing at least four synapomorphies with a late-diverging clade comprising Alioramini and Tyrannosaurini. They postulated that large Tyrannosaurus-like teeth previously identified from the Nanxiong Formation may in fact belong to a mature form of the same species as Asiatyrannus. The researchers concluded that Asiatyrannus is most parsimoniously regarded as a juvenile member of the Tyrannosaurini that is difficult to distinguish—but is potentially distinct—from Tarbosaurus. The size and proportions of the skull are almost identical to those of juvenile specimens of this genus.[5]
Paleoecology
Asiatyrannus is known from the Nanxiong Formation, which dates to the end of the Maastrichtian age of the late Cretaceous period. Large teeth indicate the presence of a large tyrannosaurid in the ecosystem that may actually be a mature form of Asiatyrannus.[7][5] Many other dinosaurs have been described from layers of the formation, including the fellow tyrannosaurid Qianzhousaurus.[2] Other theropods include therizinosaurids (Nanshiungosaurus)[8] and many oviraptorids (Banji, Corythoraptor, Ganzhousaurus, Huanansaurus, Jiangxisaurus, Nankangia, Shixinggia, and Tongtianlong).[9][10] The somphospondylan sauropods Gannansaurus and Jiangxititan are also known from the formation.[11] The formation's non-dinosaurian fauna includes crocodilians (Jiangxisuchus),[12] lizards (Chianghsia and Tianyusaurus),[13] and turtles (Jiangxichelys).[14]
The Mongolian Nemegt Formation contains a similar fauna, including the large tyrannosaurine Tarbosaurus, two species of the alioramin Alioramus, and smaller tyrannosauroids such as Bagaraatan.[15]
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References
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