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<document>
<title>Iguanodon</title>
<authors>Wikipedia</authors>
<publisher>wikipedia.org</publisher>
<publishedplace>network</publishedplace>
<publishedyear>2010</publishedyear>
<edition></edition>
<category>Cretaceous dinosaurs</category>
<section id="17818" fatherid="0" title="" lv="" priority="-1" level="1">
Iguanodon (, meaning "Iguana tooth") is a genus of ornithopod dinosaur that lived roughly halfway between the first of the swift bipedal hypsilophodontids and the ornithopods' culmination in the duck-billed dinosaurs. Many species of Iguanodon have been named, dating from the Kimmeridgian age of the Late Jurassic Period to the Cenomanian age of the Late Cretaceous Period from Asia, Europe, and North America. However, research in the first decade of the 2000s suggests that there is only one well-substantiated species: I. bernissartensis, that lived from the Barremian to the early Aptian (Early Cretaceous) in Europe, between about 130 and 120 million years ago. Iguanodon's most distinctive features were its large  spikes, which were possibly used for defence against predators and foraging for food.
Discovered in 1822 and described three years later by English geologist Gideon Mantell, Iguanodon was the second dinosaur formally named, after Megalosaurus. Together with Megalosaurus and Hylaeosaurus, it was one of the three genera originally used to define Dinosauria. A large, bulky herbivore, Iguanodon is a member of Iguanodontia, along with the duck-billed hadrosaurs. The taxonomy of this genus continues to be a topic of study as new species are named or long-standing ones reassigned to other genera.
Scientific understanding of Iguanodon has evolved over time as new information has been obtained from the fossils. The numerous specimens of this genus, including nearly complete skeletons from two well-known bonebeds, have allowed researchers to make informed hypotheses regarding many aspects of the living animal, including feeding, movement, and social behaviour.  As one of the first scientifically well-known dinosaurs, Iguanodon has occupied a small but notable place in the public's perception of dinosaurs, its artistic representation changing significantly in response to new interpretations of its remains.

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<section id="17819" fatherid="0" title="Description" lv="" priority="-2" level="1">
Iguanodon was a bulky herbivore that could shift from bipedality to quadrupedality.  The best-known species, I. bernissartensis, is estimated to have weighed about 3.08 tonnes (3.5 tons) on average, and measured about 10 metres long (32.8 ft) as an adult, with some specimens possibly as a long as 13 metres (42.6 ft). Other species were not as large; the similarly robust I. dawsoni is estimated at 8 metres long (26.2 ft), and its more lightly built contemporary I. fittoni at 6 metres (19.7 ft). This genus had a large, tall but narrow skull, with a toothless beak probably covered with keratin, and teeth like those of an iguana, but much larger and more closely packed.
The arms were long (up to 75% the length of the legs in I. bernissartensis) and robust, with rather inflexible hands built so that the three central fingers could bear weight. The s were conical spikes that stuck out away from the three main digits. In early restorations, the spike was placed on the animal's nose. Later fossils revealed the true nature of the  spikes, although their exact function is still debated. They could have been used for defense, or for foraging for food. The little finger was elongated and dextrous, and could have been used to manipulate objects. The legs were powerful, but not built for running, and there were three toes on each foot. The backbone and tail were supported and stiffened by ossified tendons, which were tendons that turned to bone during life (these rod-like bones are usually omitted from skeletal mounts and drawings). Overall, in body structure, it was not too dissimilar from its later relatives, the hadrosaurids.

</section>
<section id="17820" fatherid="0" title="Classification and origins" lv="" priority="-3" level="1">
Iguanodon gives its name to the unranked clade Iguanodontia, a very populous group of ornithopods with many species known from the Middle Jurassic to the Late Cretaceous. Aside from Iguanodon, the best-known members of the clade include Dryosaurus, Camptosaurus, Ouranosaurus, and the duck-bills, or hadrosaurs. In older sources, Iguanodontidae was shown as a distinct family. Norman, David B. "Iguanodontidae". The Illustrated Encyclopedia of Dinosaurs, 110–115. This family traditionally has been something of a wastebasket taxon, including ornithopods that were neither hypsilophodontids or hadrosaurids. In practice, animals like Callovosaurus, Camptosaurus, Craspedodon, Kangnasaurus, Mochlodon, Muttaburrasaurus, Ouranosaurus, and Probactrosaurus were usually assigned to this family. With the advent of cladistic analyses, Iguanodontidae as traditionally construed was shown to be paraphyletic, and these animals are recognised to fall at different points in relation to hadrosaurs on a cladogram, instead of in a single distinct clade. Essentially, the modern concept of Iguanodontidae currently includes only Iguanodon. Groups like Iguanodontoidea are still used as unranked clades in the scientific literature, though many traditional iguanodontids are now included in the superfamily Hadrosauroidea. Iguanodon lies between Camptosaurus and Ouranosaurus in cladograms, and is probably descended from a camptosaur-like animal. At one point, Jack Horner suggested, based mostly on skull features, that hadrosaurids actually formed two more distantly-related groups, with Iguanodon on the line to the flat-headed hadrosaurines, and Ouranosaurus on the line to the crested lambeosaurines, but his proposal has been rejected.
</section>
<section id="17821" fatherid="0" title="Discovery and history" lv="" priority="4" level="1">
<section id="17822" fatherid="17821" title="Gideon Mantell, Sir Richard Owen, and the discovery of dinosaurs" lv="" priority="1" level="2">
The discovery of Iguanodon has long been accompanied by a popular legend. The story goes that Gideon Mantell's wife, Mary Ann, discovered the first teeth of an Iguanodon in the strata of Tilgate Forest in Whitemans Green, Cuckfield, Sussex, England, in 1822 while her husband was visiting a patient. However, there is no evidence that Mantell took his wife with him while seeing patients. Furthermore, he admitted in 1851 that he himself had found the teeth. Not everyone agrees that the story is false, though. It is known from his note-books that Mantell first acquired large fossil bones from the quarry at Whitemans Green in 1820. Because also theropod teeth were found, thus belonging to carnivores, he at first interpreted these bones, which he tried to combine into a partial skeleton, as those of a giant crocodile. In 1821 Mantell mentioned the find of herbivorous teeth and began to consider the possibility that a large herbivorous reptile was present in the strata. However, in his 1822 publication Fossils of the South Downs he as yet did not dare to suggest a connection between the teeth and his very incomplete skeleton, presuming that his finds presented two large forms, one carnivorous ("an animal of the Lizard Tribe of enormous magnitude"), the other herbivorous. In May 1822 he first presented the herbivorous teeth to the Geological Society of London but the members, among which William Buckland, dismissed them as fish teeth or the incisors of a rhinoceros from a Tertiary stratum. On 23 June 1823 Charles Lyell showed some to Georges Cuvier, during a soiree in Paris, but the famous French naturalist at once discarded them as those of a rhinoceros. Though Cuvier the very next day retracted, Lyell only reported the dismissal to Mantell, who became rather diffident about the issue. In 1824 Buckland described Megalosaurus and was on that occasion invited to visit Mantell's collection. Seeing the bones on 6 March he agreed that these were of some giant saurian — though still denying it was a herbivore. Emboldened nevertheless, Mantell again sent some teeth to Cuvier, who answered on 22 June 1824 that he had determined that they were reptilian and quite possibly belonged to a giant herbivore. In a new edition that year of his Recherches sur les Ossemens Fossiles Cuvier admitted his earlier mistake, leading to an immediate acceptance of Mantell, and his new saurian, in scientific circles. Mantell tried to further corroborate his theory by finding a modern-day parallel among extant reptiles. In September 1824 he visited the Royal College of Surgeons but at first failed to find comparable teeth. However, assistant-curator Samuel Stutchbury recognised that they resembled those of an iguana he had recently prepared, albeit twenty times longer. Mantell did not describe his findings until 10 February 1825, when he presented a paper on the remains to the Royal Geological Society of London.
In recognition of the resemblance of the teeth to those of the iguana, Mantell named his new genus Iguanodon or "iguana-tooth", from iguana and the Greek word odon, odontos ("tooth"). Based on isometric scaling, he estimated that the creature might have been up to 18 metres (60 ft) long, more than the 12 metres (40 ft) length of Megalosaurus. His initial idea for a name was Iguana-saurus ("Iguana lizard"), but his friend William Daniel Conybeare suggested that that name was more applicable to the iguana itself, so a better name would be Iguanoides ("Iguana-like") or Iguanodon.Cadbury, D. (2000). The Dinosaur Hunters. Fourth Estate:London, 384 p. ISBN 1-85702-959-3. He neglected to add a specific name to form a proper binomial, so one was supplied in 1829 by Friedrich Holl: I. anglicum, which was later amended to I. anglicus. 
A better specimen was discovered in a quarry in Maidstone, Kent, in 1834, which Mantell soon acquired.  He was able to identify it as an Iguanodon from its distinctive teeth. The Maidstone slab allowed the first skeletal reconstructions and artistic renderings of Iguanodon. As such, he made some mistakes, the most famous of which was the placement of what he thought was a horn on the nose. The discovery of much better specimens in later years revealed that the horn was actually a modified . Still encased in rock, the Maidstone skeleton is currently displayed at the Natural History Museum in London. The borough of Maidstone commemorated this find by adding an Iguanodon as a supporter to their coat of arms in 1949. This specimen has become linked with the name I. mantelli, a species named in 1832 by Christian Erich Hermann von Meyer in place of I. anglicus, but it actually comes from a different formation than the original I. mantelli/I. anglicus material.
At the same time, tension began to build between Mantell and Richard Owen, an ambitious scientist with much better funding and society connections in the turbulent worlds of Reform Act-era British politics and science. Owen, a firm creationist, opposed the early versions of evolutionary science ("transmutationism") then being debated and used what he would soon coin as dinosaurs as a weapon in this conflict. With the paper describing Dinosauria, he scaled down dinosaurs from lengths of over 61 metres (200 ft), determined that they were not simply giant lizards, and put forward that they were advanced and mammal-like, characteristics given to them by God; according to the understanding of the time, they could not have been "transmuted" from reptiles to mammal-like creatures.Torrens, Hugh. "Politics and Paleontology". The Complete Dinosaur, 175–190. 
In 1849, a few years before his death in 1852, Mantell realised that Iguanodon was not a heavy, pachyderm-like animal, as Owen was putting forward, but had slender forelimbs; however, his passing  him unable to participate in the creation of the Crystal Palace dinosaur sculptures, and so Owen's vision of the dinosaurs became that seen by the public for decades. With Benjamin Waterhouse Hawkins, he had nearly two dozen lifesize sculptures of various prehistoric animals built out of concrete sculpted over a steel and brick framework; two Iguanodon, one standing and one resting on its belly, were included. Before the sculpture of the standing Iguanodon was completed, he held a banquet for twenty inside it.Norman, David B. The Illustrated Encyclopedia of Dinosaurs. p. 11.

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<section id="17823" fatherid="17821" title="Bernissart" lv="" priority="2" level="2">
The largest find of Iguanodon remains to date occurred in 1878 in a coal mine at Bernissart in Belgium, at a depth of 322 m (1056 ft).  With the encouragement of Alphonse Briart, supervisor of mines at nearby Morlanwelz, Louis Dollo, with Louis de Pauw, oversaw excavation of the skeletons and reconstructed them. At least 38 Iguanodon individuals were uncovered, most of which were adults. Many of them went on public display beginning in 1882 and are still present for viewing; 9 are displayed as standing mounts, and 19 are still in the Museum's underfloor . The exhibit makes an impressive display in the Royal Belgian Institute of Natural Sciences, in Brussels.  A replica of one of these is on display at the Oxford University Museum of Natural History and at the Sedgwick Museum in Cambridge.  Most of the remains were referred to a new species, I. bernissartensis, a larger and much more robust animal than the English remains had yet revealed, but one specimen was referred to the nebulous, gracile I. mantelli (now Dollodon bampingi). The skeletons were some of the first complete dinosaur skeletons known.  Found with the dinosaur skeletons were the remains of plants, fish, and other reptiles, including the crocodyliform Bernissartia. 
The science of conserving fossil remains was in its infancy, and was ill-equipped to deal with what soon became known as "pyrite disease". Pyrite in the bones was changing to iron sulphate, damaging the remains by causing them to crack and crumble. When in the ground, the bones were exposed to moisture that prevented this from happening, but when removed into the drier open air, the natural chemical conversion began to occur. Not knowing the true cause, and thinking it was an actual infection, the staff at the Museum in Brussels attempted to treat the problem with a combination of alcohol, arsenic, and shellac. This combination was intended to simultaneously penetrate (alcohol), kill any biological agent (arsenic), and harden (shellac) the fossils.  This treatment had the unintended effect of sealing in moisture and extending the period of damage.  Modern treatments instead involve either monitoring the humidity of fossil storage, or, for fresh specimens, preparing a special coating of polyethylene glycol that is then heated in a vacuum pump, so moisture is immediately removed and pore space is infiltrated with polyethelene glycol to seal and strengthen the fossil.
Dollo's specimens allowed him to show that Owen's prehistoric pachyderms were not correct for Iguanodon. He instead modelled the skeletal mounts after the emu and wallaby, and put the spike that had been on the nose firmly on the . He was not completely correct, but he also had the disadvantage of being faced with some of the first complete dinosaur remains. A problem that was later recognised was the bend he introduced into the tail. This organ was more or less straight, as shown by the skeletons he was excavating, and the presence of ossified tendons. In fact, to get the bend in the tail for a more wallaby or kangaroo-like posture, the tail would have had to be broken. With its correct, straight tail and back, the animal would have walked with its body held horizontal to the ground, arms in place to support the body if needed.
Excavations at the quarry were stopped in 1881, although it was not exhausted of fossils, as recent drilling operations have shown. Abstracts of Papers, Sixty-Third Annual Meeting. During World War I, when the town was occupied by German forces, preparations were made to reopen the mine for palaeontology, and Otto Jaekel was sent from Berlin to supervise. The Allies recaptured Bernissart just as the first fossiliferous layer was about to be uncovered.  Further attempts to reopen the mine were hindered by financial problems and were stopped altogether in 1921 when the mine flooded.

</section>
<section id="17824" fatherid="17821" title="To the present: Worldwide finds" lv="" priority="3" level="2">
Research on Iguanodon decreased during the early part of the 20th century as World Wars and the Great Depression enveloped Europe. A new species that would become the subject of much study and taxonomic controversy, I. atherfieldensis, was named in 1925 by R. W. Hooley, for a specimen collected at Atherfield Point on the Isle of Wight. However, what had been a European genus was now being found worldwide, with material in Africa (teeth from Tunisia and elsewhere in the Sahara), Mongolia (I. orientalis), and the United States in North America (I. ottingeri from Utah). Another North American species, from South Dakota, once assigned to Iguanodon as I. lakotaensis, has since been reclassified as the genus Dakotadon.
Iguanodon was not part of the initial work of the dinosaur renaissance that began with the description of Deinonychus in 1969, but it was not neglected for long. David B. Weishampel's work on ornithopod feeding mechanisms provided a better understanding of how it fed, and David B. Norman's work on numerous aspects of the genus has made it one of the best-known dinosaurs. In addition, a further find of numerous Iguanodon skeletons, in Nehden, Nordrhein-Westphalen, Germany, has provided evidence for gregariousness in this genus, as the animals in this areally restricted find appear to have been killed by flash floods.  At least 15 individuals, from 2 to 8 metres long (6.6 to 26.2 ft), have been found here, although at least some of them are gracile iguanodontians and belong to the related Mantellisaurus or Dollodon (described as I. atherfieldensis, at that time believed to be another species of Iguanodon).
Iguanodon material has also been used in the search for dinosaur DNA and other biomolecules. In research by Graham Embery et al., Iguanodon bones were processed to look for remnant proteins. In this research, identifiable remains of typical bone proteins, such as phosphoproteins and proteoglycans, were found in a rib.

</section>
</section>
<section id="17825" fatherid="0" title="Species" lv="" priority="5" level="1">
<section id="17826" fatherid="17825" title="" lv="" priority="-1" level="2">
Because Iguanodon is one of the first dinosaur genera to have been named, numerous species have been assigned to it.  While never becoming the wastebasket taxon several other early genera of dinosaurs became (such as Megalosaurus and Pelorosaurus), Iguanodon has had a complicated history, and its taxonomy continues to undergo revisions. Remains of the best-known species have come from Belgium, England, Germany, Spain, and France. Remains of similar animals possibly belonging to this genus have been found in Tunisia and Mongolia, and a distinct species is present in Utah, USA.  Gregory Paul has recommended limiting use of I. bernissartensis to the Bernissart finds, and using I. sp. (meaning undetermined species) for robust iguanodontian remains from Barremian-age rocks of Europe. Thus, after thorough restudy, what had been seen as a quintessentially British dinosaur may in fact be poorly known from England.
I. anglicus was the original type species, but the holotype was based on a single tooth and only partial remains of the species have been recovered since. In March 2000, the International Commission on Zoological Nomenclature changed the type species to the much better known I. bernissartensis. The original Iguanodon tooth is held at Te Papa Tongarewa, the national museum of New Zealand in Wellington, although it is not on display. The fossil arrived in New Zealand following the move of Gideon Mantell's son Walter there; after the elder Mantell's death, his fossils went to Walter.

</section>
<section id="17827" fatherid="17825" title="Species currently accepted as valid" lv="" priority="2" level="2">
Only a few of the many species assigned to Iguanodon are still considered to be valid, and only one may fall within the genus Iguanodon. I. bernissartensis, described by George Albert Boulenger in 1881, is the neotype for the genus. This species is best known for the many skeletons discovered in Bernissart, but is also known from remains across Europe. David Norman suggested that it includes the dubious Mongolian I. orientalis, but this has not been followed by other researchers.
Two species described by Richard Lydekker in the late 1800s are valid, but rarely discussed. I. dawsoni, described by Lydekker in 1889, is known from two partial skeletons found in East Sussex, England, from the middle Valanginian-age Lower Cretaceous Wadhurt Clay. I. fittoni was also described by Lydekker, in 1888. Like I. dawsoni, this species is known from the Wadhurst Clay of East Sussex.  Remains from Spain may also pertain to it. Norman (2004) wrote that three partial skeletons are known for it, but this is an error. The two species are separated on the basis of vertebral and pelvic characters, size, and build. For example, I. dawsoni was more robust than I. fittoni, with large Camptosaurus-like vertebrae featuring short neural spines, whereas I. fittoni is known for its "long, narrow, and steeply inclined neural spines". Neither of these species may actually pertain to Iguanodon.

</section>
<section id="17828" fatherid="17825" title="Reassigned species" lv="" priority="3" level="2">
Two species of Iguanodon named by Richard Owen have since been reassigned to other genera. I. hoggi (also spelled I. boggii or hoggii), named by Owen for a lower jaw from the Tithonian-Berriasian-age Upper Jurassic-Lower Cretaceous Purbeck Beds of Dorset in 1874, has been reassigned to its own genus, Owenodon. I. major, a vertebra from the Isle of Wight described by Owen in 1842 as a species of Streptospondylus, is a nomen dubium which is now thought to be a synonym of I. anglicus, although it may be its own species.
Other than the two species described by Owen which have been reassigned to other genera, fourteen other species have since been reclassified. Iguanodon albinus (or Albisaurus scutifer), described by Czech palaeontologist Antonin Fritsch (correctly Frič) in 1893, is a dubious nondinosaurian reptile now known as Albisaurus albinus. I. atherfieldensis, described by R.W. Hooley in 1925, was smaller and less robust than I. bernissartensis, with longer neural spines. It was renamed Mantellisaurus atherfieldensis in 2007. I. exogyrarum (also spelled I. exogirarum or I. exogirarus) was described by Fritsch in 1878. It is a nomen dubium based on very poor material and has been reassigned, by George Olshevsky, to Ponerosteus. I. valdensis, described by Hulke in 1879 from vertebral and pelvic remains, was from the Barremian stage of the Isle of Wight. Originally named Vectisaurus, it may be a partially grown specimen of Mantellisaurus atherfieldensis,Norman, David B. "A review of Vectisaurus valdensis, with comments on the family Iguanodontidae". Dinosaur Systematics, 147–161. or from an undetermined species of Mantellisaurus. I. gracilis, named by Lydekker in 1888 as the type species of Sphenospondylus and assigned to Iguanodon in 1969 by Rodney Steel, may belong to Mantellisaurus atherfieldensis.
I. foxii (also spelled I. foxi) was originally described by Thomas Henry Huxley in 1869 as the type species of Hypsilophodon; Owen (1873 or 1874) reassigned it to Iguanodon, but his assignment was soon overturned.I. hollingtoniensis (also spelled I. hollingtonensis), described by Lydekker in 1889, has been regarded as a synonym of I. fittoni,, although this assessment has not been evaluated in detail.  Another specimen assigned to I. hollingtonensis by Richard Owen in 1874, with an unusual combination of hadrosaurid-like lower jaw and very robust forelimb, may represent an unnamed taxon. I. prestwichii (also spelled I. prestwichi), described by John Hulke in 1880, has been reassigned to Camptosaurus prestwichii. I. seeleyi (also spelled I. seelyi), described by Hulke two years after I. prestwichii, has been synonymised with I. bernissartensis, although this has been disputed. I. suessii, described by Emanuel Bunzel in 1871, has been reassigned to Mochlodon suessi.
I. lakotaensis was described by David B. Weishampel and Philip R. Bjork in 1989. The only well-accepted North American species of Iguanodon, I. lakotaensis was described from a partial skull from the Barremian-age Lower Cretaceous Lakota Formation of South Dakota.  Its assignment has been controversial. Some researchers suggest that it was more basal than I. bernissartensis, and related to Theiophytalia,Brill, Kathleen and Kenneth Carpenter. "A description of a new ornithopod from the Lytle Member of the Purgatoire Formation (Lower Cretaceous) and a reassessment of the skull of Camptosaurus."  Horns and Beaks, 49–67. but David Norman has suggested that it was a synonym of I. bernissartensis. Gregory S. Paul has since given the species its own genus, Dakotadon.
Iguanodon mantelli (also spelled I. manteli or I. mantellii), described by Christian Erich Hermann von Meyer in 1832, is actually based on the same material as I. anglicus. Several skeletons, however, including the Maidstone specimen and one of the Bernissart skeletons have been assigned here over the years, and their attribution is not complete. The gracile Bernissart skeleton, for example, has been reassigned, first to Mantellisaurus atherfieldensis, and upon further review, to its own genus and species, Dollodon bampingi. I. orientalis, described by A. K. Rozhdestvensky in 1952, was based on poor material, but a skull with a distinctive arched snout that had been assigned to it was renamed Altirhinus kurzanovi in 1998. At the same time, I. orientalis was considered to be a nomen dubium indistinguishable from I. bernissartensis. Harry Seeley described I. phillipsi in 1869, but later reassigned it to Priodontognathus.

</section>
<section id="17829" fatherid="17825" title="Dubious species" lv="" priority="4" level="2">
Five Iguanodon species are considered to be nomina dubia or undescribed. I. anglicus, described by Friedrich Holl in 1829, is the original type species of Iguanodon, but, as discussed above, was replaced by I. bernissartensis. In the past, it has been spelled as I. angelicus (Lessem and Glut, 1993) and I. anglicum (Holl, 1829 emend. Bronn, 1850).  It is known from teeth from the Valanginian-Barremian-age Lower Cretaceous Tilgate Forest of East Sussex, England. I. hillii, coined by Edwin Tully Newton in 1892 for a tooth from the early Cenomanian Upper Cretaceous Lower Chalk of Hertfordshire, is an early hadrosaurid of some sort.Horner, John R., David B. Weishampel and Catherine A. Forster. "Hadrosauridae". The Dinosauria, pp 438–463. "I. mongolensis" (Whitfield, 1992) is a nomen nudum from a photo caption in a book, of remains that would later be named Altirhinus.
I. ottingeri, described by Peter Galton and James A. Jensen in 1979, is a nomen dubium based on teeth from the possibly Aptian-age lower Cedar Mountain Formation of Utah. I. praecursor (also spelled I. precursor), described by E. Sauvage in 1876 from teeth from an unnamed Kimmeridgian (Late Jurassic) formation in Pas-de-Calais, France, is actually a sauropod, sometimes assigned to Neosodon, although the two come from different formations.Upchurch, Paul, Paul M. Barrett, and Peter Dodson. "Sauropoda". The Dinosauria
Finally, several other poorly known genera and species are included with Iguanodon without being separate species, although their assignment is less certain with the renaming of I. atherfieldensis. These include Heterosaurus neocomiensis (Cornuel, 1850), Hikanodon (Keferstein, 1834), and Therosaurus (Fitzinger, 1840), and the species "Streptospondylus" recentior (Owen, 1851), "Cetiosaurus" brachyurus, and part of "C." brevis (Owen, 1842; "C." brevis is a chimera). The nomen nudum "Proiguanodon" (van den Broeck, 1900) also belongs here, and possibly the very obscure "Streptospondylus" grandis (Owen, 1851) and meyeri (Owen, 1854).

</section>
</section>
<section id="17830" fatherid="0" title="Palaeobiology" lv="" priority="-6" level="1">
<section id="17831" fatherid="17830" title="Feeding and diet" lv="" priority="1" level="2">
One of the first details noted about Iguanodon was that it had the teeth of a herbivorous reptile, although there has not always been consensus on how it ate. As Mantell noted, the remains he was working with were unlike any modern reptile, especially in the toothless, scoop-shaped form of the lower jaw symphysis, which he found best compared to that of the two-toed sloth and the extinct ground sloth Mylodon. He also suggested that Iguanodon had a prehensile tongue which could be used to gather food, like a giraffe. More complete remains have shown this to be an error; for example, the hyoid bones that supported the tongue are heavily built, implying a muscular, non-prehensile tongue used for moving food around in the mouth. The giraffe-tongue idea has also been incorrectly attributed to Dollo via a broken lower jaw.Norman, D.B. (1985). The Illustrated Encyclopedia of Dinosaurs, 115.
Iguanodon teeth are, as the name suggests, like those of an iguana, but larger.  Unlike hadrosaurids, which had columns of replacement teeth, Iguanodon only had one replacement tooth at a time for each position.  The upper jaw held up to 29 teeth per side, with none at the front of the jaw, and the lower jaw 25; the numbers differ because teeth in the lower jaw are broader than those in the upper. Because the tooth rows are deeply inset from the outside of the jaws, and because of other anatomical details, it is believed that, as with most other ornithischians, Iguanodon had some sort of cheek-like structure, muscular or non-muscular, to retain food in the mouth.Fastovsky, D.E., and Smith, J.B. "Dinosaur paleoecology." The Dinosauria, 614–626.
The skull was structured in such a way that as it closed, the bones holding the teeth in the upper jaw would bow out. This would cause the lower surfaces of the upper jaw teeth to rub against the upper surface of the lower jaw's teeth, grinding anything caught in between and providing an action that is the rough equivalent of mammalian chewing. Because the teeth were always replaced, the animal could have used this mechanism throughout its life, and could eat tough plant material. Additionally, the front ends of the animal's jaws were toothless and tipped with bony nodes, both upper and lower, providing a rough margin that was likely covered and lengthened by a keratinous material to form a cropping beak for biting off twigs and shoots. Its food gathering would have been aided by its flexible little finger, which could have been used to manipulate objects, unlike the other fingers.
Exactly what Iguanodon ate with its well-developed jaws is not known. The size of the larger species, such as I. bernissartensis, would have allowed them access to food from ground level to tree foliage at 4–5 metres high (13–16.5 ft). A diet of horsetails, cycads, and conifers was suggested by David Norman, although iguanodonts in general have been tied to the advance of angiosperm plants in the Cretaceous due to the dinosaurs' inferred low browsing habits. Angiosperm growth, according to this hypothesis, would have been encouraged by iguanodont feeding because gymnosperms would be removed, allowing more space for the weed-like early angiosperms to grow.Bakker, R.T. "When Dinosaurs Invented Flowers". The Dinosaur Heresies, 179–198 The evidence is not conclusive, though. Whatever its exact diet, due to its size and abundance, Iguanodon is regarded as a dominant medium to large herbivore for its ecological communities. In England, this included the small predator Aristosuchus, larger predators Eotyrannus, Baryonyx, and Neovenator, low-feeding herbivores Hypsilophodon and Valdosaurus, fellow "iguanodontid" Mantellisaurus, the armoured herbivore Polacanthus, and sauropods like Pelorosaurus.Weishampel, D.B., Barrett, P.M., Coria, R.A., Le Loeuff, J., Xu Xing, Zhao Xijin, Sahni, A., Gomani, E.M.P., and Noto, C.R. "Dinosaur Distribution". The Dinosauria, 517–606.

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<section id="17832" fatherid="17830" title="Posture and movement" lv="" priority="2" level="2">
Early fossil remains were fragmentary, which led to much speculation on the posture and nature of Iguanodon. As discussed, Iguanodon was initially portrayed as a quadrupedal horn-nosed beast. However as more bones were discovered, Mantell observed that the forelimbs were much smaller than the hindlimbs. His rival Owen was of the opinion it was a stumpy creature with four pillar-like legs. The job of overseeing the first lifesize reconstruction of dinosaurs was initially offered to Mantell, who declined due to poor health, and Owen's vision subsequently formed the basis on which the sculptures took shape. Its bipedal nature was revealed with the discovery of the Bernissart skeletons. However, it was depicted in an up posture, with the tail dragging along the ground, acting as the third leg of a tripod.
During his re-examination of Iguanodon, David Norman was able to show that this posture was unlikely, due to the presence of a long tail stiffened with ossified tendons. To get the tripodal pose, the tail would literally have to be broken. Putting the animal in a horizontal posture makes many aspects of the arms and pectoral girdle more understandable. For example, the hand is relatively immobile, with the three central fingers grouped together, bearing hoof-like phalanges, and able to hyperextend. This would  have allowed them to bear weight.  The wrist is also relatively immobile, and the arms and shoulder bones robust. These features all suggest that the animal spent time on all fours. 
Furthermore, it appears that Iguanodon became more quadrupedal as it got older and heavier; juvenile I. bernissartensis have shorter arms than adults (60% of hindlimb length versus 70% for adults). When walking as a quadruped, the animal's hands would have been held so that the palms faced each other, as shown by iguanodontian trackways and the anatomy of this genus' arms and hands. The three toed pes (foot) of Iguanodon was relatively long, and when walking, both the hand and the foot would have been used in a digitigrade fashion (on the fingers and toes). The maximum speed of Iguanodon has been estimated at 24 km/h (14.9 mph), which would have been as a biped; it would not have been able to gallop as a quadruped.
Large three-toed footprints are known in Early Cretaceous rocks of England, particularly Wealden beds on the Isle of Wight, and these trace fossils were originally difficult to interpret. Some authors associated them with dinosaurs early on. In 1846, E. Tagert went so far as to assign them to an ichnogenus he named Iguanodon, and Samuel Beckles noted in 1854 that they looked like bird tracks, but might have come from dinosaurs. The identity of the trackmakers was greatly clarified upon the discovery in 1857 of the hind leg of a young Iguanodon, with distinctly three-toed feet, showing that such dinosaurs could have made the tracks. Despite the lack of direct evidence, these tracks are often attributed to Iguanodon. A trackway in England shows what may be an Iguanodon moving on all fours, but the foot prints are poor, making a direct connection difficult. Tracks assigned to the ichnogenus Iguanodon are known from locations including places in Europe where  the body fossil Iguanodon is known, to Spitsbergen, Svalbard, Norway.

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<section id="17833" fatherid="17830" title="Thumb spike" lv="" priority="3" level="2">
The  spike is one of the most well-known features of Iguanodon. Although it was originally placed on the animal's nose by Mantell, the complete Bernissart specimens allowed Dollo to correctly place it on the hand, as a modified . (This would not be the last time a dinosaur's modified  claw would be misinterpreted; Noasaurus, Baryonyx, and Megaraptor are examples since the 1980s where an enlarged  claw was first put on the foot, as in dromaeosaurids.)
This  is typically interpreted as a close-quarters stiletto-like weapon against predators, although it could also have been used to break into seeds and fruits, or against other Iguanodon. One author has suggested that the spike was attached to a venom gland, but this has not been accepted, as the spike was not hollow, nor were there any grooves on the spike for conducting venom.

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<section id="17834" fatherid="17830" title="Possible social behaviour" lv="" priority="-4" level="2">
Although sometimes interpreted as the result of a single catastrophe, the Bernissart finds instead are now interpreted as recording multiple events. According to this interpretation, at least three occasions of mortality are recorded, and though numerous individuals would have died in a geologically short time span (?10–100 years), this does not necessarily mean these Iguanodon were herding animals.
An argument against herding is that juvenile remains are very uncommon at this site, unlike modern cases with herd mortality. They more likely were the periodic victims of flash floods whose carcasses accumulated in a lake or marshy setting. The Nehden find, however, with its greater span of individual ages, more even mix of Dollodon or Mantellisaurus to Iguanodon bernissartensis, and confined geographic nature, may record mortality of herding animals migrating through rivers.
Unlike other purported herding dinosaurs (especially hadrosaurs and ceratopsids), there is no evidence that Iguanodon was sexually dimorphic, with one gender appreciably different from the other. At one time, it was suggested that the Bernissart I. "mantelli", or I. atherfieldensis (Dollodon and Mantellisaurus, respectively) represented a gender, possibly female, of the larger and more robust, possibly male, I. bernissartensis. However, this is not supported today.

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<section id="17835" fatherid="0" title="In popular culture" lv="" priority="7" level="1">
Since its description in 1825, Iguanodon has been a feature of worldwide popular culture. Two lifesize reconstructions of Iguanodon built at the Crystal Palace in London in 1852 greatly contributed to the popularity of the genus. Their  spikes were mistaken for horns, and they were depicted as elephant-like quadrupeds, yet this was the first time an attempt was made at constructing full-size dinosaur models.
Several motion pictures have featured Iguanodon. In the Disney film Dinosaur, an Iguanodon named Aladar served as the protagonist with three other iguanodonts as other main characters; a loosely related ride of the same name at Disney's Animal Kingdom is based around bringing an Iguanodon back to the present.  Iguanodon is one of the three dinosaur genera that inspired Godzilla; the other two were Tyrannosaurus and Stegosaurus. Iguanodon has also made appearances in some of the many Land Before Time films, as well as episodes of the television series.
Aside from appearances on the silver screen, Iguanodon has also been featured on the television documentary miniseries Walking with Dinosaurs (1999) produced by the BBC, and played a starring role in Sir Arthur Conan Doyle's book, The Lost World as well as featuring in an episode of the Discovery Channel documentary, Dinosaur Planet. It also was present in Bob Bakker's Raptor Red (1995), as a Utahraptor prey item. A main belt asteroid, , has been named 9941 Iguanodon in honour of the genus.
Because it is both one of the first dinosaurs described and one of the best-known dinosaurs, Iguanodon has been well-placed as a barometer of changing public and scientific perceptions on dinosaurs.  Its reconstructions have gone through three stages: the elephantine quadrupedal horn-snouted reptile of the Victorians; a bipedal but still fundamentally reptilian animal using its tail to prop itself up; and finally, its current, more agile and dynamic representation, able to shift from two legs to all fours. The second representation dominated the twentieth century, but was slowly overturned during the 1960s.

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<section id="17836" fatherid="0" title="References" lv="" priority="-8" level="1">
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<section id="17837" fatherid="0" title="External links" lv="" priority="-9" level="1">
Category:Cretaceous dinosaurs
Category:Dinosaurs of Europe
Category:Iguanodonts
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