iguanodon

/i gwah"neuh don', i gwan"euh-/, n.

a plant-eating dinosaur of the genus Iguanodon that lived in Europe early in the Cretaceous Period and grew to a length of from 15 to 30 ft. (4.5 to 9 m) and walked erect on its hind feet.

[ < NL (1825) < Sp iguan(a) IGUANA + Gk odón, var. of ODO_{S TOOTH]}

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▪ dinosaur genus

 large herbivorous dinosaurs (dinosaur) found as fossils from the Late Jurassic (Jurassic Period) and Early Cretaceous periods (Cretaceous Period) (159 million to 99 million years ago) in a wide area of Europe, North Africa, North America, Australia, and Asia; a few have been found from Late Cretaceous deposits of Europe and southern Africa.

      Iguanodon was the largest, best known, and most widespread of all the iguanodontids (family Iguanodontidae), which are closely related to the hadrosaurs, or duck-billed dinosaurs. Iguanodon was 9 metres (30 feet) long, stood nearly two metres tall at the hip, and weighed four to five tons. The animal probably spent its time grazing while moving about on four legs, although it was able to walk on two. Iguanodontid forelimbs had an unusual five-fingered hand: the wrist bones were fused into a block; the joints of the thumb were fused into a conelike spike; the three middle fingers ended in blunt, hooflike claws; and the fifth finger diverged laterally from the others. Furthermore, the smallest finger had two small additional phalanges, a throwback to more primitive dinosaurian configuration. The teeth were ridged and formed sloping surfaces whose grinding action could pulverize its diet of low-growing ferns (fern) and horsetails (horsetail) that grew near streams and rivers. Most bones of the skull and jaws were not tightly fused but instead had movable joints that allowed flexibility when chewing tough plant material.

      In 1825 Iguanodon became the second species to be described scientifically as a dinosaur, the first having been Megalosaurus. Iguanodon was named for its teeth, whose similarity to those of modern iguanas (iguana) also provided the dinosaur's discoverer, the English physician Gideon Mantell (Mantell, Gideon Algernon), with the first clue that dinosaurs had been reptiles (reptile). In his first reconstruction of the incomplete remains of Iguanodon, Mantell restored the skeleton in a quadrupedal pose with the spikelike thumb perched on its nose. This reconstruction persisted in London's famous Crystal Palace dinosaur sculptures by Waterhouse Hawkins (1854) until many complete skeletons were found in Bernissart, Belgium, during the 1880s. Reconstructions of the Belgian skeletons mistakenly placed the animal in an upright, kangaroo-like stance with its tail on the ground—a misconception not corrected until the late 20th century, when a posture based upon a nearly horizontal backbone was adopted.

      The fossil remains of many individuals have been found, some in groups, which suggests that iguanodontids traveled in herds. Fossilized tracks of iguanodontids are also relatively common and are widespread in Late Jurassic and Early Cretaceous deposits.

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