Qianshanosuchus

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Kingdom:Animalia
Phylum:Chordata
Class:Reptilia
Qianshanosuchus
Temporal range: Paleocene
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Archosauria
Order: Crocodilia
Genus: Qianshanosuchus
Boerman et al., 2022
Species:
Q. youngi
Binomial name
Qianshanosuchus youngi
Boerman et al., 2022

Qianshanosuchus is a genus of basal crocodyloid from the Paleocene of the Qianshan Basin, China. The fossil material, which includes an incomplete skull and parts of the lower jaw, show various features usually associated with juvenile crocodiles alongside various unique traits that were used to erect a new genus. It is the first and only basal crocodyloid currently known from the Paleocene of China, which had previously only yielded alligatoroids and planocraniids. Its presence in this part of the world and its basal position to species of the genus Asiatosuchus supports the idea that crocodyloids dispersed from Asia into Europe. Qianshanosuchus only includes a single species, Qianshanosuchus youngi.[1]

Qianshanosuchus is known from only a single specimen, IBCAS QS15, an incomplete skull and an associated part of the mandible. Based on the small size of the holotype and several anatomical traits, it is thought to preserve a juvenile specimen. The material was collected near Xialou village in the Qianshan Basin of China by a joint expedition of Belgian and Chinese researchers. Preparation was handled by the Museum of Natural Sciences of Belgium and the fossils were curated by the Institute of Botany, Chinese Academy of Sciences.[1]

The genus name derives from the Qianshan Basin and the Greek 'soukhos' for "crocodile". The species is named after Yang Zhongjian, also known as Chung-Chien Young.[1]

Description

The skull of Qianshanosuchus is small, measuring only 9.7 cm (3.8 in) from the tip of the snout to the back of the skull, one of several traits that indicate that the material belonged to a juvenile. The maxillary foramen, a hole in the skull for the fifth cranial nerve, is notably enlarged. The suture where the squamosal and parietal bones meet is situated on a ridge and an acute notch stretches over the parietal and supraoccipital, the later of which is largely exposed on the skull table. The dorsal edge of the orbits is raised and on the mandible the surangular features a prominent ridge on the lateral side of the bone.[1]

Of five premaxillary teeth, only the last is preserved and shows a smooth surface with no visible ridges. While only this tooth is present in the premaxillae, based on the size of the alveoli the third and fourth were the largest in this part of the jaw. The maxillae preserve only six alveoli, but based on the size of them and the bad preservation of the rest of the bone, it is likely that in life the animal would have had between eight and sixteen maxillary teeth. The preserved teeth are thought to represent the first, second, third, fifth and possibly the ninth tooth of the maxilla. All of them are angled labially (outwards) and show slight lateral compression, which is typically seen in juvenile crocodilians but also found in adult planocranids.[1]

Several other features of the skull are also indicative of the fact that the material that forms Qianshanosuchus belonged to a juvenile. This includes the relative size of the orbits compared to the full skull and similarly the size of the skull table compared to the total skull width. Overall, the orbits take up three quarters of the skulls width and one quarter of its length. The supratemporal fenestrae are shallow and widely spaced as seen in the juveniles of modern species, the skull lacks the pronounced ornamentation that is typical for adult crocodiles and various other characters related to the teeth, frontal bone and other elements likewise suggest that the specimen was not yet mature at the time of its death. In spite of these variable features however, those deemed diagnostic for Qianshanosuchus were determined to be unaffected by ontogeny in modern crocodilians. The only exception regards the upturned margins of the orbits, which remain unchanged in some species but disappear with age in others.[1]

Phylogeny

Biogeography

References

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