Hypselospinus

Quality 0.50 · 1 view · Updated 2 months ago

Extinct genus of dinosaurs

title: "Hypselospinus" type: doc version: 1 created: 2026-02-28 author: "Wikipedia contributors" status: active scope: public tags: ["ankylopollexia", "dinosaur-genera", "valanginian-dinosaurs", "fossil-taxa-described-in-2010", "taxa-named-by-david-b.-norman", "dinosaurs-of-the-united-kingdom"] description: "Extinct genus of dinosaurs" topic_path: "geography/united-kingdom" source: "https://en.wikipedia.org/wiki/Hypselospinus" license: "CC BY-SA 4.0" wikipedia_page_id: 0 wikipedia_revision_id: 0

::summary Extinct genus of dinosaurs ::

Darwinsaurus evolutionis? Paul, 2012
Huxleysaurus hollingtoniensis Paul, 2012

Hypselospinus is a genus of iguanodontian dinosaur which was first described as a species of Iguanodon (I. fittoni) by Richard Lydekker in 1889, the specific name honouring William Henry Fitton.

History and naming

In the 1880s, the Natural History Museum, London, purchased multiple collections of fossils discovered by Charles Dawson from the region Hastings. Among these collections of specimens were multiple individuals identified as species of Iguanodon by British palaeontologist Richard Lydekker, from the Early Cretaceous Wadhurst Clay Formation. The first of these specimens, NHMUK R.1635, was found in Shornden Quarry over distance of 50 yard, and includes a partial and believed to be from a single individual. As the specimen was smaller than and younger than the similar and nearby species Iguanodon dawsoni and the pelvis showed some differences, Lydekker chose to name the new species Iguanodon fittoni in 1889, with the species name honouring William Henry Fitton who had worked in the Early Cretaceous strata of England.

As well as I. fittoni, Lydekker identified another new species of Iguanodon, I. hollingtoniensis, from among the material collected by Dawson in Hollington Quarry near Hastings. Also from the Wadhurst Clay Formation, Lydekker identified a series of specimens (NHMUK R.1148, R.1629, and R.1632) as being from the same individual. While he had previously considered NHMUK R.1148, a partial right leg, as I. dawsoni, based on its smaller size and differences in the he chose to name the new species in 1889. Lydekker also assigned to I. hollingtoniensis a single individual bearing the specimen numbers NHMUK R.811, R.811b, and R.604, and identified the partial skeleton NHMUK R.33 as belonging to either I. fittoni or I. hollingtoniensis though he could not identify which. ::figure[src="https://upload.wikimedia.org/wikipedia/commons/9/9a/Hypselospinus_bone_NHM.jpg" caption="Metatarsal III foot bone of specimen NHMUK R1148n (formerly assigned to its own genus, ''Huxleysaurus'')"] ::

Lydekker elaborated further upon his classifications of Iguanodon fittoni and I. hollingtoniensis in 1890, describing them as members of a "proiguanodont" group along with I. dawsoni. The type specimen of I. fittoni was identified as a series of NHMUK R.1635 to R.1635d, all purchased from Dawson in 1889 and including portions of the sacrum, pelvis, a and three teeth. The type specimens of I. hollingtoniensis included NHMUK R.1148, R.1629, R.1632, R.1632a, and R.1632b, covering many regions of the skeleton including the neck, tail, and both fore- and hindlimbs. NHMUK R.604, R.811, R.811b, R.1634, and R.1636 were all referred, coming from either the Hollington or Shornden Quarries and including regions of the skeleton also found in the types. Many specimens were previously referred to I. dawsoni, but considered by Lydekker as more similar to I. hollongtoniensis. Lydekker also illustrated the ilium and femur of I. fittoni and I. hollingtoniensis in comparison to the other species of Iguanodon.

British palaeontologist David B. Norman was the first to suggest that I. fittoni and I. hollingtoniensis could represent the same taxon in 1987, with I. fittoni taking priority as it was described one page before I. hollingtoniensis. Together, I. fittoni and I. dawsoni would be the two iguanodonts from the Wadhurst Clay Formation, both found at Shornden and other sites and from the same Valanginian age. The material of I. fittoni, including I. hollingtoniensis, was misidentified as three partial skulls and jaws in 1990 and 2004 reviews. Not all authors agreed on the inclusion of I. hollingtoniensis within I. fittoni, with American palaeontologist Gregory S. Paul in 2008, and British palaeontologist Peter M. Galton in 2009 retaining the species as separate, and as potentially belonging in a new genus separate from Iguanodon.

In May 2010 the fossils comprising Hypselospinus were by David Norman reclassified as a separate genus, among them the holotype BMNH R1635, consisting of a left ilium, a sacrum, tail vertebrae and teeth. The generic name is derived from Greek hypselos, "high" and Latin spina, "thorn", in reference to the high vertebral spines. Later that same year, a second group of scientists independently re-classified I. fittoni into a new genus they named Wadhurstia, which thus is a junior objective synonym of Hypselospinus. Hypselospinus lived during the lower Valanginian stage, around 140 million years ago. A contemporary of Barilium (also once thought to be a species of Iguanodon), Hypselospinus was a lightly built iguanodontian estimated at 6 metres (19.7 ft) long. The species Iguanodon fittoni was described from remains discovered in 1886 alongside an unnamed ichthyosaur in the lower Valanginian-age Lower Cretaceous Wadhurst Clay of Shornden, East Sussex, England. Remains from Spain may also pertain to it. Norman (2004) wrote that three partial skeletons are known for it, but this is an error.

Hypselospinus is separated from Barilium on the basis of vertebral and pelvic characters, size, and build. For example, Barilium was more robust than Hypselospinus, with large Camptosaurus-like vertebrae featuring short neural spines, whereas Hypselospinus is known for its "long, narrow, and steeply inclined neural spines".

References

Lydekker, R.. (1888). "Catalogue of the Fossil Reptilia and Amphibia in the British Museum (Natural History). Part I. Containing the Orders Ornithosauria, Crocodilia, Dinosauria, Squamata, Rhynchocephalia, and Proterosauria". Taylor & Francis.
Lydekker, R.. (1889). "Notes on New and other Dinosaurian Remains". Geological Magazine.
Lydekker, R.. (1890). "Catalogue of the Fossil Reptilia and Amphibia in the British Museum (Natural History). Part IV. Containing the Orders Anomodontia, Ecaudata, Caudata, and Labyrinthodontia; and Supplement". Taylor & Francis.
Lydekker, R.. (1890). "Contributions to our knowledge of the dinosaurs of the Wealden and the sauropterygians of the Purbeck and Oxford Clay". Quarterly Journal of the Geological Society.
(1990). "The Dinosauria". University of California Press.
Blows, W. T.. (1997). "Lower and Middle Cretaceous Terrestrial Ecosystems". New Mexico Museum of Natural History and Science.
Norman, David B.. (2004). "The Dinosauria". University of California Press.
Naish, Darren. (2008). "Dinosaurs of Great Britain and the role of the Geological Society of London in their discovery: Ornithischia". Journal of the Geological Society, London.
Paul, G.S.. (2008). "A revised taxonomy of the iguanodont dinosaur genera and species". Cretaceous Research.
Galton, P.M.. (2009). "Notes on Neocomian (Late Cretaceous) ornithopod dinosaurs from England – ''Hypsilophodon'', ''Valdosaurus'', "Camptosaurus", "Iguanodon" – and referred specimens from Romania and elsewhere". Revue de Paléobiologie.
Norman, David B.. (2010). "A taxonomy of iguanodontians (Dinosauria: Ornithopoda) from the lower Wealden Group (Cretaceous: Valanginian) of southern England". Zootaxa.
Carpenter, K. and Ishida, Y. (2010). "[http://www.ucm.es/info/estratig/JIG/vol_content/vol_36_2/36_2_145_164_Carpenter.pdf Early and “Middle” Cretaceous Iguanodonts in Time and Space.]{{dead link. (July 2016)

::callout[type=info title="Wikipedia Source"] This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page. ::