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Extinct species of reptile From Wikipedia, the free encyclopedia
Hungarosaurus tormai (meaning 'Hungarian lizard' from the Latin Hungaria 'Hungary' and Greek σαυρος / 'sauros' 'lizard'), is a herbivorous nodosaurid ankylosaur from the Upper Cretaceous (Santonian) Csehbánya Formation of the Bakony Mountains of western Hungary. It is the most completely known ankylosaur from the Cretaceous of Europe.
| Hungarosaurus Temporal range: Santonian, | |
|---|---|
| |
| Right dentary | |
Scientific classification  | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Dinosauria |
| Clade: | †Ornithischia |
| Clade: | †Thyreophora |
| Clade: | †Ankylosauria |
| Family: | †Nodosauridae |
| Subfamily: | †Nodosaurinae |
| Clade: | †Struthiosaurini |
| Genus: | †Hungarosaurus Ősi, 2005 |
| Species: | †H. tormai |
| Binomial name | |
| †Hungarosaurus tormai Ősi, 2005 | |
Hungarosaurus walked on four legs and its body was covered with hundreds of osteoderms. The length of mature specimens was about 4–4.8 metres (13–16 ft) . Like other nodosaurids, it was a herbivore.
The species was named by Attila Ősi in 2005. The generic name is derived from Hungary and the Greek sauros, lizard. The specific name honours András Torma, the amateur paleontologist who discovered the fossil site in 2000.
Four specimens of Hungarosaurus tormai are known, all collected from an open-pit bauxite mine near the village of Iharkút, Veszprém County, in the Bakony Mountains (Transdanubian Range) of western Hungary. The quarry exposes the Csehbánya Formation (which overlies the Halimba Formation, also Cretaceous in age), which is a floodplain and channel deposit consisting largely of sandy clays and sandstone beds. The specimen designated as the holotype is MTM Gyn/404 (in the collections of the Magyar Természettudományi Múzeum, Budapest, Hungary) and consists of 450 bones, including portions of the skull (premaxilla, left prefrontal, left lacrimal, right postorbital, jugal and quadratojugal, left frontal, pterygoid, vomer, the right quadrate and a fragment of the left quadrate, basioccipital, one hyoid), an incomplete right mandible, three cervical vertebrae, six dorsal vertebrae, ten caudal vertebrae, ossified tendon fragments, three cerival and thirteen dorsal ribs, five chevrons, the left scapulocoracoid, right scapula, portions of the right manus, a partial pelvis, and more than one hundred osteoderms.[1]
Hungarosaurus was a small nodosaur, measuring 4–4.8 metres (13–16 ft) in length and weighing 650–1,000 kilograms (1,430–2,200 lb).[2][3] The skull of this dinosaur is ornamented and estimated to have been 32–36 centimetres in length.[4]
Cladistic analysis on the taxon indicates that it is a derived member of the Nodosauridae, along with Struthiosaurus (another European nodosaurid).
The studies show that Hungarosaurus is slightly more advanced than Struthiosaurus, but more primitive than the North American nodosaurids Silvisaurus, Sauropelta and Pawpawsaurus. This was supported by cladistic analysis, which suggests that it is a basal member of the family Nodosauridae.
The exposure of the Csehbánya Formation that produced Hungarosaurus tormai has also yielded remains of bony fishes, turtles, lizards, crocodiles, and pterosaurs, along with teeth from a diminutive dromaeosaurid-like theropod and a Rhabdodon-like ornithopod.[1]
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