Langbahn Team – Weltmeisterschaft

Comptonatus

Comptonatus
Temporal range: Early Cretaceous,
Barremian–Aptian
Speculative life reconstruction
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Ornithischia
Clade: Neornithischia
Clade: Ornithopoda
Family: Iguanodontidae
Genus: Comptonatus
Lockwood, Martill & Maidment, 2024
Species:
C. chasei
Binomial name
Comptonatus chasei
Lockwood, Martill & Maidment, 2024

Comptonatus (meaning "the Compton thunderer") is a genus of ornithopod dinosaur from the early Cretaceous period. Its remains are known from the Wessex Formation in England. The type and only species is C. chasei.

Discovery and naming

The holotype specimen, IWCMS 2014.80, was excavated in September–October 2013, close to where a Valdosaurus specimen was recovered the previous year. It is the most complete ornithopod dinosaur found on the Isle of Wight since Mantellisaurus in 1914.[1][2]

Comptonatus was described as a new genus and species of iguanodontian dinosaur in 2024. The generic name, Comptonatus, combines the name of the location Compton with the Latin tonatus, meaning "thundered", and has the intended meaning of "the Compton thunderer", in reference to its discovery location and large size. The specific name, chasei, honours the late Nick Chase, who won the Palaeontological Association's Mary Anning Award in 2018 and discovered the specimen.[1][3]

Classification

Comptonatus was entered into a phylogenetic analysis using the dataset of the description of the contemporary Brighstoneus.[4] It was found to be in a clade with Iguanodon, Barilium, and Mantellisaurus, all from southern England, which has been termed the Iguanodontidae. The cladogram from the analysis is shown below:[1]

Paleoenvironment

Comptonatus is one of several iguanodontians known from the Isle of Wight, distinct from Iguanodon, Brighstoneus, and Mantellisaurus. The deposition of the Wessex Formation likely spans several million years, and so it is unlikely to have been contemporaneous with all of these other taxa. The Wessex Formation had a warm and semi-arid Mediterranean climate, formed on alluvial meander plains. Forests on higher ground north of the floodplain consisted of Pinophyta, Ginkgophyta, Pteridophyta, Cycadophyta. Forest fires and floods were common occurrences, resulting in the formation of plant debris beds.[4]

References