Horshamosaurus

Horshamosaurus
Temporal range: Barremian

Cretaceous

Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Archosauria
Superorder: Dinosauria
Order: Ornithischia
Suborder: Thyreophora
Infraorder: Ankylosauria
Genus: Horshamosaurus
Blows, 2015
species
  • Horshamosaurus rudgwickensis Blows, 2015 (type species Polacanthus rudgwickensis)

Horshamosaurus is a genus of herbivorous ankylosaurian dinosaur from the Early Cretaceous of England.

Discovery

In 1985, at the marl quarry of the Rudgwick Brickworks Company near Rudgwick in West Sussex, fossils were dug up of dinosaurs. These were secured by two volunteers of the Horsham Museum: Morris Zdzalek and Sylvia Standing. After 1988, the finds were exhibited in the museum as Iguanodon bones. Subsequently neurologist William T. Blows, an amateur paleontologist who already had extensively published on the subject of armoured dinosaurs, determined that the bones were not iguanodontian but instead represented ankylosaurian remains.

In 1996, on basis of the finds, a new species of the genus Polacanthus, Polacanthus rudgwickensis, was named and described by Blows. The specific name refers to the provenance from Rudgwick.[1]

The material, holotype HORSM 1988.1546, was found in a layer of gray-green marl beds of the lower Weald Clay Formation dating from the Barremian age, over 125 million years old. It is fragmentary and includes two incomplete dorsal vertebrae, part of a front tail vertebra, bone fragments of other vertebrae, a partial left scapulocoracoid of the shoulder girdle, the distal end of a humerus, a nearly complete right tibia, rib fragments, and two osteoderms.[1]

In 2015, Blows made it a separate genus Horshamosaurus, the generic name referring to Horsham. Its type species is Polacanthus rudgwickensis. The combinatio nova is Horshamosaurus rudgwickensis.[2]

Description

Horshamosaurus seems, at roughly five metres length, to have been about 30% longer than the type species of Polacanthus, Polacanthus foxii and differs from it in numerous characters of the vertebrae and dermal armour. The centrum facets of the back and tail vertebrae have a round instead of a heart-shaped profile. The transverse processes of the vertebrae each have two ridges at their undersides delimiting a depression and gradually merging with the vertebral body. The transverse processes of the front tail vertebrae merge with the neural arch, forming a distinctive ridge. The "pseudoacromion" is located close to the front edge of the shoulder blade. The rear ribs are large and tall instead of rather slender. The shinbone is relatively longer. The osteoderm spikes on the back have a circular base of which the front underside is excavated but the rear underside solid, instead of an oval base with a uniformly concave underside. One of the osteoderms seems to have been part of the back armour and is large and flat with a concave underside; plates of such a type have not been discovered with Polacanthus foxii.

Phylogeny

Horshamosaurus is not a sister species of Polacanthus. In 2015, Blows did not place Horsamosaurus in a Polacanthidae but in a more derived position in the Ankylosauria.

References

  1. 1 2 Blows W.T. (1996) "A new species of Polacanthus (Ornithischia; Ankylosauria) from the Lower Cretaceous of Sussex, England". Geological Magazine, 133 (6): 671–682
  2. Blows, W.T., 2015, British Polacanthid Dinosaurs – Observations on the History and Palaeontology of the UK Polacanthid Armoured Dinosaurs and their Relatives, Siri Scientific Press, 220 pp
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