Rhabdodon

and paralectotype dentaries Rhabdodon is known from southern France, although fragmentary remains from eastern Spain have been assigned to the genus. Rhabdodon was large compared to its nearest relatives, and indeed one recent paper (Ősi et al., 2012) determined it is larger than the basal rhabdodontid status; from this they suggested that it actually experienced gigantism on the "mainland" and not insular dwarfism as previous suggested. The type species was originally named under two spellings by Matheron (1869), Rhabdodon priscum and Rabdodon priscum. While later authors adopted Rhabdodon as the correct spelling, this genus name was originally established for a snake in a thesis by Fleischmann (1831), which led to some researchers abandoning the name in favor of Mochlodon. In 1986, the Swiss paleontologist Winand Brinkmann submitted an application for the International Code of Zoological Nomenclature (ICZN) to suppress this previous use by Fleischmann (1831) and to amend the specific name to priscus. The approval of this petition by the ICZN in 1988 conserved and formalized the binomen Rhabdodon priscus for the type species. In 1991, the French paleontologists Eric Buffetaut and Jean Le Loueff named the second species R. septimanicus from the Argiles et Grès à Reptiles Formation. In 2025, the Polish paleontologists Łukasz Czepiński and Daniel Madzia reassigned this species to its own genus, Obelignathus. ==Classification==

'' The cladogram below is based on the analysis of Ösi et al. (2012): ==Paleobiology==

Rhabdodon was probably an herbivore in Cretaceous Europe. Carnivorous dinosaurs in the ecosystem included the abelisaurid Arcovenator and the paravian Pyroraptor. Isotope analysis shows that Rhabdodon, along with its smaller cousin Zalmoxes, ate C3 plants. ==Palaeoenvironment==

Rhabdodon is known from a specimen from the Marnes Rouges Inférieures Formation. The known material includes a dentary and many other postcranial remains. More specifically, it is known from the Bellevue layer, which has produced many vertebrate fossils. Even though it produced many vertebrates, the formation only has a scarce record of plants and invertebrates. The non-dinosaurian vertebrates consist of Lepisosteus, an indeterminate turtle, and a crocodile. Dinosaurian fauna from the Marnes Rouges Inférieures Formation include Ampelosaurus, an animal classified as Dromaeosauridae indet., and an indeterminate ankylosaur. Villalba de la Sierra Formation Rhabdodon sp. is from the latest Cretaceous aged Lo Hueco region in the Villalba de la Sierra Formation. A study shows that the area around Lo Hueco dates to the late Campanian and early Maastrichtian, although a more recent study revised the later date to the latest Maastrichtian. The study showed that Lo Hueco was near the coast of the Tethys Sea, Many dinosaurs have been found in the Villalba de la Sierra Formation, including Rhabdodon sp. They consist of possible Lirainosaurus remains, Ampelosaurus atacis, unknown basal euornithopods, probable ankylosaurians, one undetermined dromaeosaurine, and one unknown velociraptorine. The plants known from the formation are represented by carbonized branches and leaves. Invertebrates are solely known from bivalves and gastropods. Fishes from the formation include lepisosteids, and unidentified actinopterygians and teleosteans. Turtle fossils are very common, but only two different groups have been identified, the bothremydids Polysternon and Rosasia, along with an undetermined Pancryptodiran. Squamate lizards are known only from a few undetermined specimens, and eusuchian crocodiles are known from a specimen with similarities to Allodaposuchus and Musturzabalsuchus. == References ==