Temporal range: Early Cretaceous, 125 Ma
|Reconstructed skeleton, World Museum Liverpool|
Hutt, Martill & Barker, 1996
Neovenator (nee-o-ven-a-tor) which means "new hunter" is a genus of allosauroid dinosaur. At the time of its discovery on the Isle of Wight, UK, it was the best-known large carnivorous dinosaur from the Early Cretaceous of Europe. Neovenator was at first considered possibly a new species of Megalosaurus.
Neovenator measured approximately 7.6 meters (25 feet) in length, and was of a gracile build, weighing 1000–2000 kg. Specimen MIWG 4199 indicates an individual with a possible length of about ten meters (33 feet), but it only consists of a toe phalanx.
The various scientific descriptions of Neovenator have indicated some distinguishing traits. The nostril is twice as long as it is high. The praemaxilla in the snout bears five teeth. The maxilla is pierced by a large maxillary fenestra, the diameter of which equals a sixth of the length of the tooth row. The tooth crown equals a quarter of the tooth length, thus including the root. The toe claws have a groove on top. Both praemaxillae are connected by an extra pen-in-socket connection. The front joint surface of the intercentrum of the axis, the second neck vertebra, is transversely widened. The odontoid process of the axis has small openings along the side edge of the front facet. The neural process of the axis has a single small opening in the side. The rear neck vertebrae are fused with their neck ribs. On the eighth and ninth neck vertebrae, at the parapophysis, the lower rib joint facet, the internal camellate structure of the bone is visible. At the front neck vertebrae the undersides are formed as sharp keels which are not inset from the lateral sides. At the front back vertebrae, the hypapophyses, the lower swellings of the front facet edges, are formed like low mounds. On the rear back vertebrae the facets of the joint processes are continued sideways as curved flanges. The shoulder joint is wider transversely than long, measured from the front to the rear. The notch on the underside of the front blade of the ilium has a shelf at the inner side. The "feet" of the ischia are connected at their fronts but diverge at their rears. The head of the thighbone is obliquely directed to the front, to above and to the inside. On the thighbone the lesser trochanter has a robust ridge on its outer side. On the thighbone the fourth trochanter has a depression in the form of a thumbprint located to the outside of its upper limit. The front underside of the thighbone is nearly flat, only showing a short vertical groove between the lower condyles. The lower shinbone shows a oval rough area at the inner side. The top of the outer malleolus of the shinbone is pinched from the front to the rear. The outer front bulge of the top surface of the shinbone has a spur pointing to below. In the foot, the outer side of the second metatarsal has a hollow surface to contact the third metatarsal.
Several traits that once were thought to be unique or apomorphic for Neovenator, subsequent research showed to have been shared by other theropods. The nostrils are large but not uncommonly so. Having pneumatised rear back vertebrae is normal for carcharodontosaurids. Elevated paired nasal crests are shared with Allosaurus. Denticles continuing over the tooth apex are today known from other species.
In 2015, it was reported that the front of the snout of Neovenator contains a complex system of neurovascular canals, functioning as sensory organs. This trait is also known from Spinosauridae and was there explained as an adaptation for searching prey in water. It was doubted however, whether Neovenator used its system for the same purpose.
Discovery and species
The first bones of the Neovenator were discovered in the summer of 1978, when a storm made part of the Grange Chine collapse. Rocks containing fossils fell to the beach of Brighstone Bay on the southwestern coast of the Isle of Wight. The rocks consisted of a plant debris bed within the variegated clays and marls of the Wessex Formation dating from the Barremian stage of the Early Cretaceous, about 125 million years ago. They were first collected by the Henwood family and shortly afterwards by geology student David Richards. Richards sent the remains to the Museum of Isle of Wight Geology and the British Museum of Natural History. In the latter institution paleontologist Alan Jack Charig determined that the bones belonged to two kinds of animal: Iguanodon and some theropod. The "iguanodon", later referred to Mantellisaurus, generated the most interest and in the early 1980s a team was sent by the BMNH to secure more of its bones. On that occasion an additional theropod tail vertebra was discovered. Several amateur paleontologists, among them Keith and Jenny Simmonds, now began to search for additional remains of the predator. Ultimately, the total of secured bones included the snout, teeth, a front lower jaw, most of the vertebral column, ribs, belly ribs, chevrons, the left shoulder girdle, pelvis bones and a hindlimb. These were accessioned under numbers BMNH R10001 and MIWG 6348. They equalled approximately 70% of the skeleton. In 1985, excavations undertaken by Dr Steve Hutt of the MIWG revealed two vertebrae of a second individual, specimen MIWG.5470. In 1987, Jenny Simmonds found a third skeleton, containing vertebra and pelvic bones, specimen MIWG.6352. A fourth individual is represented by specimen IWCMS 2002.186, consisting of a lower jaw, vertebrae and limb elements. In 1990 the material, then considered a possible new species of Megalosaurus, was provisionally described by Hutt. Having mistaken the ischium of MIWG 6352 for a pubic bone, Hutt suggested this specimen represented a separate species.
In 1996, Steve Hutt, David Martill and Michael Barker named and described the type species Neovenator salerii. The generic name Neovenator means "new hunter" from the Greek neo~, "new" and Latin venator, "hunter". The specific name salerii honours the land owners of the site, the Salero family. In view of the large number of individuals involved in the discovery process, it was considered improper to single out one of them as discoverer. The holotype is the skeleton accessioned as BMNH R10001 and MIWG 6348.
In 1999, Hutt dedicated his, unpublished, master thesis to Neovenator.
At the time that it was described, by Steve Hutt, Martill and Barker in 1996, it was considered the only known allosaurid in Europe. However, further studies suggested it had more in common with the advanced carcharodontosaurid group of allosaurs, and several studies including a detailed examination of the species by Benson, Carrano and Brusatte in 2010 suggest that it is closely related to the Carcharodontosauridae (in a group called Carcharodontosauria), but is actually closer to the megaraptorans, together with them forming the family Neovenatoridae. Other studies have supported Neovenator being a carcharodontosaurid, and megaraptorans being tyrannosauroids.
Cladogram after Novas et al., 2013
Fossil remains of Neovenator have been found on the Isle of Wight off southern England, and were first discovered in the 20th century. Neovenator perhaps existed alongside other dinosaurs found in the Wessex Formation of the early Cretaceous period, such as Baryonyx, Polacanthus and Iguanodon. The holotype bones were mixed with those of the plant-eater Mantellisaurus and in the dig site also remains of fishes, amphibians, lizards, pterosaurs and Goniopholididae were present. Neovenator was one of the apex predators of its day.
The holotype of Neovenator salerii had many pathologies. The authors of the genus list them as "midcaudal vertebrae fusions, healed fractures of mid-caudal vertebra transverse processes; osteophytes affecting pedal phalanges, healed gastralia rib fractures, some forming false joints... [and] scapula fracture."
- "Neovenator - paleofiles.com".
- Dodson P., Weishampel D. B. & Osmólska H., The Dinosauria, 2nd edition (2004), University of North Carolina Press, p. 104.
- S. Hutt, D.M. Martill, and M.J. Barker, 1996, "The first European allosauroid dinosaur (Lower Cretaceous, Wealden Group, England)", Neues Jahrbuch für Geologie und Paläontologie Monatshefte 1996(10): 635-644
- Naish, D., Hutt S. and Martill, D., 2001, "Saurischian dinosaurs 2: Theropods". In: Martill D. and Naish D. (eds.), Dinosaurs of the Isle of Wight The Palaeontological Association, pp 242-309
- Brusatte S.L., Benson R.B.J., Hutt S., 2008, The osteology of Neovenator salerii (Dinosauria: Theropoda) from the Wealden Group (Barremian) of the Isle of Wight, Monograph of the Palaeontographical Society 162(631) 166 pp
- Barker, C., Dyke, G., Naish, D., Newham, E. and Katsamenis, O., 2015, "Complex neurovascular network in the rostrum of Neovenator salerii", SVPCA 2015 abstracts, 78
- Hutt, S., Simmonds, K. & Hullman, G., 1990, "Predatory dinosaurs from the Isle of Wight", Proceedings of the Isle of Wight Natural History and Archaeological Society, 9: 137-146
- Hutt, S.C. 1999. Neovenator salerii: A new theropod dinosaur from the Wealden of the Isle of Wight: its status and significance for Theropod evolution. A thesis submitted for the award of degree of Master of Philosophy (unpublished). University of Portsmouth
- Benson, R.B.J., Carrano, M.T and Brusatte, S.L. (2010). "A new clade of archaic large-bodied predatory dinosaurs (Theropoda: Allosauroidea) that survived to the latest Mesozoic." Naturwissenschaften, 97:71-78 . doi:10.1007/s00114-009-0614-x
- Zanno, L. E.; Makovicky, P. J. (2013). "Neovenatorid theropods are apex predators in the Late Cretaceous of North America". Nature Communications 4: 2827. Bibcode:2013NatCo...4E2827Z. doi:10.1038/ncomms3827. PMID 24264527.
- Novas, Fernando E. (2013). "Evolution of the carnivorous dinosaurs during the Cretaceous: The evidence from Patagonia". Cretaceous Research 45: 174–215. doi:10.1016/j.cretres.2013.04.001.
- Molnar, R. E., 2001, Theropod paleopathology: a literature survey: In: Mesozoic Vertebrate Life, edited by Tanke, D. H., and Carpenter, K., Indiana University Press, p. 337-363.
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