Lurdusaurus ("heavy lizard") is a genus of massive and unusually shaped iguanodont dinosaur from the Elrhaz Formation in Niger. It contains one species, L. arenatus. The formation dates to the Early Cretaceous, roughly 112 million years ago.
Lurdusaurus has a highly atypical body plan for an iguanodont, with a small skull, long neck, rotund torso, and powerful forelimbs and claws (the thumb-pike is remarkably enormous), somewhat reminiscent of a ground sloth. Lurdusaurus is estimated to have been long and high when on all-fours, but its stomach would have been only off the ground. It may have weighed , conspicuously heavy for an iguanodontid this size.
Paleontologist Thomas R. Holtz Jr. speculated Lurdusaurus may have behaved much like a hippo. It lived in a forested, riverine environment alongside the iguanodonts Elrhazosaurus and Ouranosaurus, the sauropod Nigersaurus, an undescribed titanosaurid, the spinosaurid Suchomimus, the carcharodontosaurid Eocarcharia, the abelisaurid Kryptops, and the noasaurid Afromimus. The site also yielded several crocodylomorph species and a pterosaur.
Lurdusaurus may have had 12 to 14 neck vertebrae. Therefore, the maximum length of the neck is . The neck vertebrae are about the same size as the dorsal vertebrae (the torso, before the sacrum and pelvis), whereas those of European iguanodonts 85–90% the size of the dorsals. Because Iguanodon has 28 presacral vertebrae, Lurdusaurus potentially had at least 14 dorsals. This would make the neck proportionally quite long, as long as the dorsal series. Compared to European iguanodonts, the dorsal centra are proportionally larger and have shorter neural spines (which project straight up from the centrum) and less steep transverse processes (which project up obliquely). Like all derived iguanodonts, the sternum is hatchet-shaped, with a rod-shaped projection caudolaterally (tailwards towards the side). The sacrum, based on the scars on the ilium begotten from sacral ribs, may have measured . Lurdusaurus could have had 15 proximal caudal vertebra (tail vertebrae which bear transverse processes), which would have represented a third of the entire tail series.
This would equate to a tail, and a total body length of . It may have been tall at the hips. Based on the length of the ribs, the stomach may have been less than off the ground when standing (on all-fours). Based on the circumferences of the limbs – for the humerus and for the femur – Taquet and Russell estimated that the holotype weighed approximately , conspicuously heavy for an ornithopod this size. In 2016, however, Gregory S. Paul proposed a significantly lower size estimate of in length and in body mass. The headward dorsal ribs are preserved in their original positions, and show the torso was rather rotund. The diverging wings of the ilia and horizontally-orientated tailward dorsal indicate a flat back about across.
The limbs are exceptionally massive and proportionally stout. The forelimbs are 60% the size of the hindlimbs. The first metacarpal, radiale, and intermedium were together into a massive block, similar to other ankylopollexians such as Iguanodon and Ouranosaurus. Like Camptosaurus but unlike derived iguanodonts, the metacarpals (except for the thumb) were short and dumbbell-like as opposed to long and narrow. Compared to Camptosaurus, the (claws) are flatter. The hand features a massive thumb spike. The pelvis is proportionally short but powerful, somewhat reminiscent of a pelvis. The femur slightly recurves toward the midline like in ceratopsians, and is flattened anteroposteriorly (from front to back) like in . The heavily built fourth trochanter is located on the bottom half of the femur, like Iguanodon but unlike Mantellisaurus and Ouranosaurus. The tibia is incredibly short relative to the femur, respectively vs. . The were too short to make contact with each other, and there was likely a fleshy pad to support the weight.
In 2004, British paleontologist David B. Norman placed it outside of Iguanodontidae but still within the clade Styracosterna, which he defined as containing all iguanodonts with a hatchet-like sternum and flattened hand claws. He agreed Lurdusaurus is a more derived iguanodont. In 2005, Chinese paleontologist You Hai-Lu and colleagues suggested that the newly discovered and massively built Lanzhousaurus from China was closely related to Lurdusaurus, and the former was basal to the latter. He classified both of them as basal styracosterns.
In 2008, American freelance researcher Gregory S. Paul argued that because Lanzhousaurus has a much deeper prepubic process, the two genera are probably not closely allied, though such hypotheses are wholly unverifiable without more complete remains. Paul agreed that Lurdusaurus is more basal to Iguanodontidae based on its short, broad hands and massive thumb spike, but he noted that the contemporary and more derived hadrosauriform Ouranosaurus has similar hand morphology. Therefore, Lurdusaurus could be a basal hadrosauriform, but Paul could not resolve the matter any further until more complete remains are discovered. In 2009, American paleontologist Peter Galton placed Lurdusaurus at the base of Styracosterna and closely allied it with the Chinese Equijubus. He classified more derived iguanodonts into the new clade Iguanodontea. In 2012, Taquet agreed with Paul that it falls outside Iguanodontidae, but was also unsure how exactly Lurdusaurus relates with other iguanodonts. The phylogenetic analysis of Karen E. Poole in 2022 found that Lurdusaurus formed a clade with other iguanodonts with robust forelimbs, Hypselospinus and Barilium.
Taquet and Russell compared the fortified hand with its massive thumb spike to a ball-and-chain flail, and believed it was primarily used for defense.
Lurdusaurus was recovered from the Elrhaz Formation, and lived alongside the iguanodonts Ouranosaurus and Elrhazosaurus, the sauropod Nigersaurus, an undescribed titanosaurid, the spinosaurid Suchomimus, the carcharodontosaurid Eocarcharia (likely a chimaera including spinosaurid bones), the abelisaurid Kryptops, and the noasaurid Afromimus. The Gadoufaoua site has also yielded an Ornithocheiridae pterosaur, and the Anatosuchus, Araripesuchus, Stolokrosuchus, and the giant Sarcosuchus. It dates to roughly 112 million years ago during the Early Cretaceous at the Aptian–Albian boundary. Geologically, it is composed of almost entirely cross-bedding fluvial sandstone (the sediments were deposited by rivers), intermittently interrupted by migrating sand . The presence of Nigersaurus suggests widespread forests with soft understory vegetation, such as immature or .
Classification
Paleoecology
See also
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