page_title: Abelisauridae
section_title: Distribution
hierarchical_section_title: Abelisauridae / Distribution
caption_attribution_description: English: Sketch of Abelisaurus comahuensis, a theropod Dinosaur which has been placed into its own taxon, the Abelisauridae, among several other genera. Deutsch: Skizze von Abelisaurus comahuensis, ein theropoder Dinosaurier, der gemeinsam mit mehreren anderen Gattungen in ein eigenes Taxon, die Abelisauridae, gestellt wurde.
context_page_description: Abelisauridae is a family of ceratosaurian theropod dinosaurs. Abelisaurids thrived during the Cretaceous period, on the ancient southern supercontinent of Gondwana, and today their fossil remains are found on the modern continents of Africa and South America, as well as on the Indian subcontinent and the island of Madagascar. Reports based on isolated teeth show the occurrence in the Late Jurassic of Portugal, and the confirmed existence of European Abelisaurids comes from the Late Cretaceous of France with Arcovenator. Abelisaurids first appear in the fossil record of the early middle Jurassic period, and at least two genera survived until the end of the Mesozoic era 66 million years ago.
  Like most theropods, abelisaurids were carnivorous bipeds. They were characterized by stocky hind limbs and extensive ornamentation of the skull bones, with grooves and pits. In many abelisaurids, such as Carnotaurus, the fore limbs are vestigial, the skull is shorter, and bony crests grow above the eyes.
context_section_description: Abelisauroids are typically regarded as a Cretaceous group, though the earliest abelisaurid remains are known from the Middle Jurassic of Argentina (classified as the species Eoabelisaurus mefi) and possibly Madagascar (fragmentary remains of an unnamed species); possible abelisaurid remains (an isolated left tibia, right femur and right tibia) were also discovered in Late Jurassic Tendaguru Beds in Tanzania. Abelisaurid remains are mainly known in the southern continents, which once made up the supercontinent of Gondwana. When first described in 1985, only Carnotaurus and Abelisaurus were known, both from the Late Cretaceous of South America. Abelisaurids were then located in Late Cretaceous India (Indosuchus and Rajasaurus) and Madagascar (Majungasaurus), which were closely connected for much of the Cretaceous. It was thought that the absence of abelisaurids from continental Africa indicated that the group evolved after the separation of Africa from Gondwana, around 100 million years ago. However, the discovery of Rugops and other abelisaurid material from the middle of the Cretaceous in northern Africa disproved this hypothesis. Mid-Cretaceous abelisaurids are now known from South America as well, showing that the group existed prior to the breakup of Gondwana. In 2014, the description of Arcovenator escotae from southern France provided the first indisputable evidence of the presence of Abelisaurids in Europe. Arcovenator presents strong similarities with the Madagascan Majungasaurus and Indian abelisaurids, but not with the South American forms. Arcovenator, Majungasaurus, and Indian forms are united in the new clade Majungasaurinae.
caption: Illustration of Abelisaurus
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