Sauroniops

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Sauroniops
Temporal range: Late Cretaceous, 100 Ma
Sauroniops holotype.png
The holotype specimen of Sauroniops pachytholus, left frontal bone MPM 2594.
Scientific classification e
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Order: Saurischia
Suborder: Theropoda
Family: Carcharodontosauridae
Genus: Sauroniops
Cau et al., 2012
Type species
Sauroniops pachytholus
Cau et al., 2012

Sauroniops is a genus of predatory basal carcharodontosaurid theropod dinosaur known from the Late Cretaceous (Cenomanian stage) of Morocco.[1]

In the early twenty-first century a collector donated a dinosaur skull bone to the Italian Museo Paleontologico di Montevarchi. He had acquired the specimen from a Moroccan fossil dealer, who again had bought the piece from local fossil hunters near Taouz. Its exact provenance is therefore uncertain. Later research showed that it presented a new species that was in 2012 reported and described by Andrea Cau, Marco Dalla Vecchia and Matteo Fabbri.[2]

The same year, 2012, the specimen was by the same authors formally named in a subsequent publication as the type species Sauroniops pachytholus. The generic name has the intended meaning of "Eye of Sauron", a demonic entity from the Lord of the Rings fantasy novel by J.R.R. Tolkien, combining its name with a Classical Greek ὄψ, ops, "eye". Like in the novels the corporeal presence of Sauron had largely been limited to a single searching eye, Sauroniops is only known from a single bone above the eye socket. The specific name is derived from Greek παχύς, pachys, "thick", and θόλος, tholos, "round building with conical roof", in reference to the thick vaulted skull roof.[1]

The holotype, specimen MPM 2594, had probably been recovered from the Kem Kem Beds dating from the Cenomanian. It consists of a left frontal bone.[1]

Description[edit]

Location of fossil

Sauroniops was a large bipedal predator. The describers established several unique traits, differentiating Sauroniops from its relatives, such as Carcharodontosaurus which is found in the same layers. The nasal bone has an area of contact with the frontal bone over 40% of the latter's length. The frontal has in the left front corner a thick vaulted area. On the front upper rim the frontal has a trapezoid facet to contact the prefrontal, which is no part of the upper rim of the eye socket, and is separated from the facet for the lacrimal bone by a thin vertical ridge. The contact area with the lacrimal is D-shaped, extremely large and has four times the height of the facet with the postorbital bone. On the rear inner side of the frontal an elevated rim is present that is joint to the front vaulted area by a saddle-shaped depression and more towards the front midline of the skull continues in a series of rugosities.[1]

The frontal has a preserved length of 186 millimetres. Near the contact with the lacrimal the bone is extremely thickened to a height of seventy-three millimetres and vaulted; a second thick area is present at the rear separated from the first by a hollow surface. Such a thickening of the skull roof is more typical of the Abelisauridae in which group however, it is the postorbital that shows the phenomenon. The authors explained the thickening as an adaptation for display or to strengthen the skull for intraspecific head-butting.[1]

The holotype of Sauroniops was originally interpreted as belonging to a derived member of the Carcharodontosauridae. A more extensive cladistic analysis in the naming paper showed a more basal position in the same group as a sister species of Eocarcharia. The similarities to the abelisaurids would then be convergences.[1]

See also[edit]

References[edit]

  1. ^ a b c d e f Cau, Andrea, Fabio M. Dalla Vecchia, Matteo Fabbri (2013). "A thick-skulled theropod (Dinosauria, Saurischia) from the Upper Cretaceous of Morocco with implications for carcharodontosaurid cranial evolution". Cretaceous Research. 40: 251–260. doi:10.1016/j.cretres.2012.09.002. 
  2. ^ Cau, A.; Dalla Vecchia, F.M.; Fabbri, M., 2012, "Evidence of a new carcharodontosaurid from the Upper Cretaceous of Morocco", Acta Palaeontologica Polonica 57(3): 661– 665