|Two Wealden dryosaurids Valdosaurus canaliculatus, argued below to be striking and exciting animals that we should all be enthused about, shown here milling about a Lower Cretaceous woodland, not doing very much. Prints of this image are available here.|
|Mounted skeleton of the Jurassic dryosaurid Dysalotosaurus lettowvorbecki in the Humboldt Museum's excellent dinosaur hall. Photo by Masur, from Wikimedia Commons. Beige.|
The Jurassic-Cretaceous clade Dryosauridae contains animals which, at first glance, represent the mean of dinosaur extremes. Most of these animals, early offshoots of the ornithopod group Iguanodontia, are small or medium-sized, at 3-4 m long. They have fairly short, unremarkable ornithopod skulls and small grasping hands which are, well, quite a lot like those of other small-ish ornithopods. They possess no horns, claws or even particularly arresting teeth, their jaw tips being entirely toothless and cheek teeth, as with most ornithopods, being leaf-shaped and coarsely serrated. This restricted them to a diet of leaves and other herbage, and there's not even any strong hints of omnviory. In short, they aren't especially cute, aren't really spectacular, and, to look at one, it's hard to find a truly distinctive, memorable feature. Perhaps this is why the only time they're given decent palaeoartistic renditions is when they're being pursued by a more striking theropod, and are relegated to bit-parts and cameo roles in most dinosaur books and palaeodocumentaries.
You knew there was a 'but' coming
As usual, appearances can be deceiving. There's actually a lot more going on with these dinosaurian plain Janes than casual glances may suggest. If you stare at a skeleton of a dryosaurid long enough, the pronounced difference in their fore and aft proportions becomes inescapable. The head, neck, forelimbs and torso belong to much smaller dinosaurs than their legs and tail, which are proportionally much longer and more robust than we'd expect from their anterior skeleton. This enlarged posterior region does not seem to reflect expansion of the gut either, as it does in some other herbivorous dinosaur species. Rather, the pelvic bones betraying the depth of the belly are fairly shallow, suggesting the legs and tail are long for the sake of being long, not to accommodate increased body size or torso girth. Of further note are dryosaurid feet, which are not only surprisingly long and gracile but also possess a mere three toes, a contrast to the primitive ornithopod condition of four. Their femora have a very long, finger-like fourth trochanter (the variably shaped process on the posterior surface of dinosaur femora which anchored posterior hindlimb muscles) and a very large and prominent scar occurs where the famous caudofemoralis musculature anchored to the thigh. As in all dinosaurs, this muscle ran to the anterior portion of the tail (discussion here), the elongation and deepening of which permitted a great deal of room for its attachment.
Put together, these femoral and caudal features are clear indicators of large hindlimb retractor muscles and, along with the svelte body and long legs, betray the habit of very rapid running. Indeed, the cursorial features of dryosaurids are so marked that they were probably among the swiftest of all ornithischians, a trait which may explain their conspicuous lack of ornament, armour and weaponry compared to other dinosaurs. Such elaborations are not without use of course, but they are just extra weight for a running animal. Thus, rather than thinking of dryosaurid skeletons as boring, we should view them as the bones of lithe, streamlined, athletes. I wonder if we'd consider these animals dinosaurian Mr. Averages if we could see them in life, their running abilities likely making them very striking and conspicuous animals in many Jurassic and Cretaceous ecoystems.
Britain's Cretaceous dryosauid: Valdosaurus
Dryosauridae was a widespread group with fossils occurring in Africa, Europe, North America and New Zealand. One British dryosaurid, the Wealden Supergroup taxon Valdosaurus, has become particularly interesting in recent years. Bones ultimately referable to this genus were described from the Wessex Formation, Isle of Wight, as early as 1888 by Richard Lydekker. They were not recognised as being Dryosaurus-like until the 1970s however, the decade which also Valdosaurus canaliculatus receive its name (Galton 1977). A second Valdosaurus species was erected for Nigerian material by Galton and Taquet (1977), but has since been moved to its own genus, Elrhazosaurus. It took a while to appreciate that dryosaurids were a unique radiation of ornithopods rather than merely oversized versions of Hypsilophodon, with the first inclinations of this idea only appearing in the 1980s. Somewhat surprisingly, the monophyly of Dryosauridae was untested for many decades, but has recently been borne out under phylogenetic analysis (e.g. McDonald et al. 2010; Barrett et al. 2011). Alleged Valdosaurus material from Spain and Romania seemed to extend the range of this animal across Europe, but these referrals have not withstood scrutiny: Valdosaurus remains UK-only for the time-being.
|Holotype femur of Valdosaurus compared to those of other small ornithopods. Note the size of the scar for M. caudofemoralis, 'p', in Valdosaurus. Figure and caption from Galton and Taquet 1977.|
Valdosaurus: apocalypse survivor?
What makes Valdosaurus especially interesting and unique among Wealden dinosaurs is its longevity. The Wealden dinosaur fauna is essentially divided into two groups: a 'lower' and 'upper' assemblage. The 'upper' contains the most widely known taxa, animals such as Iguanodon, Polacanthus, Baryonyx, Hypsilophodon, Neovenator and the like. These animals occur in rocks dating to the Hauterivian and Barremian, about 133-125 Ma. The 'lower' fauna features slightly lesser known taxa: Barilium, Hylaeosaurus, Pelorosaurus and so on, all of which are of slightly older, late Berriasian-Valangian vintage (138-133 Ma). The transition between these faunas is not continuous, with a series of poorly-fossiliferous Hauterivian-aged strata - representing about 4 million years - occurring between more productive Wealden rocks. William Blows has proposed across several papers that this gap may not merely be an artefact of sampling (although this remains possible), but a low-level extinction event that wiped out the 'lower' fauna and allowed the 'upper' assemblage to repopulate (e.g. Blows 1998). Not all agree that this apocolyptic interpretation is the most likely explanation of the Hauterivian Wealden dinosaur gap - some argue that we just need to look harder for more bones. Whatever, something clearly caused a lot of upset for the Wealden dinosaur fauna in the Hauterivian, resulting in significant reorganisation of dinosaur faunas by late Hauterivian-Barremian stages: old taxa disappeared, and new ones - sometimes entirely different clades - replaced them.
How does Valdosaurus fit into this? Although classically part of the 'upper' Wealden assemblage, Valdosaurus is now known to occur in the 'lower' fauna (e.g. Blows 1998; Naish and Martill 2008; Barrett et al. 2011). This makes it the only dinosaur to span the Hauterivian gap, suggesting it lived through whatever turned out the older Wealden dinosaurs and brought in the new. It must be stressed that the older Valdosaurus remains are not terribly complete and may not be V. canaliculatus proper, but they are extremely similar to Valdosaurus remains from the 'upper' Wealden and at worst, they represent a very close relative, perhaps a direct ancestor. Of further interest here are recent reconsiderations of Valdosaurus/dryosaurid abundance within the Wealden. Dryosaurs were once considered rare in these deposits, but ongoing appraisals of British Lower Cretaceous dinosaurs suggest they were far more abundant than once realised, and populous enough to question the dominance of iguanodonts in Wealden herbivore palaeoecology (Barrett et al. 2011). Given that Valdosaurus represents a good chunk of the Wealden dryosaur material, we may take this as a sign that it was not only a long-lived taxon, but also one that had a strong foothold in Wealden habitats.
The longevity and abundance of Valdosaurus may see it being considered one of the greatest 'success stories' of Britain's Lower Cretaceous dinosaurs, and the implications of its success to Wealden palaeoecology undoubtedly make it one of the more interesting members of the assemblage. A key question - why did it persevere when all other species didn't? - now hangs over this unassuming animal's head. With work on the Wealden fauna constantly ongoing, it seems like a case of 'watch this space' to see just how our new perception of Wealden dryosaurids will influence broader interpretations of Britain's Lower Cretaceous dinosaurs. Exciting times indeed, then, and a far cry from the perception of Valdosaurus and dryosaurids as easily-forgotten, 'average' dinosaurs: at least one of them is, from a certain perspective, one of the most interesting dinosaurs in the UK.
- Barrett, P. M., Butler, R. J., Twitchett, R. J., & Hutt, S. (2011). New material of Valdosaurus canaliculatus (Ornithischia: Ornithopoda) from the Lower Cretaceous of southern England. Special Papers in Palaeontology, 86: 131–163.
- Blows, W. T. (1998). A review of Lower and Middle Cretaceous dinosaurs of England. New Mexico Museum of Natural History and Science Bulletin, 14, 29-38.
- Galton, P. M., (1977). The Upper Jurassic dinosaur Dryosaurus and a Laurasia-Gondwana connection in the Upper Jurassic. Nature, 268(5617): 230-232
- Galton, P. M., & Taquet, P. (1982). Valdosaurus, a hypsilophodontid dinosaur from the Lower Cretaceous of Europe and Africa. Geobios, 15(2), 147-159.
- McDonald, A. T., Kirkland, J. I., DeBlieux, D. D., Madsen, S. K., Cavin, J., Milner, A. R., & Panzarin, L. (2010). New basal iguanodonts from the Cedar Mountain Formation of Utah and the evolution of thumb-spiked dinosaurs. PloS one, 5(11), e14075.
- Naish, D., & Martill, D. M. (2008). Dinosaurs of Great Britain and the role of the Geological Society of London in their discovery: Ornithischia. Journal of the Geological Society, 165(3), 613-623.