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Rhynchosauria
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Rhynchosauria
Rhynchosaurs are a group of extinct herbivorous Triassic archosauromorph reptiles, belonging to the order Rhynchosauria. Rhynchosaurs are distinguished by their triangular skulls and elongated, beak like premaxillary bones. Rhynchosaurs first appeared in the Early Triassic, reaching their broadest abundance and a global distribution during the Carnian stage of the Late Triassic, before dying out early in the succeeding Norian stage.
Rhynchosaurs were herbivores, and at times abundant (in some fossil localities accounting for 40 to 60% of specimens found), with stocky bodies and a powerful beak. Early primitive forms, like Mesosuchus and Howesia, were generally small, typically lizard-like in build, and had skulls rather similar to the early diapsid Youngina, except for the beak and a few other features. Later and more advanced genera grew to up to two meters in length. The hind feet were equipped with massive claws, presumably for digging up roots and tubers by backwards scratching of the hind limbs. Rhynchosaurs probably had a semi-erect posture (intermediate between most reptiles, which have a sprawling posture, and dinosaurs and mammals, which acquired an erect posture with a narrow stance).
The skulls of later rhynchosaurs were short, broad, and triangular, becoming much wider than long in the most advanced forms like Hyperodapedon. The toothless premaxilla bone, at the tip of the snout, extended outwards and downwards to form the upper beak. The broad skull had a deep cheek region which would have accommodated powerful jaw muscles. The lower jaw was also deep, and when the mouth was closed it clamped firmly into the maxilla (upper edge of the jaw), like the blade of a penknife closing into its handle. This scissors-like action would have enabled rhynchosaurs to cut up tough plant material.
The teeth were unusual; those in the maxilla and palate were modified into broad tooth plates, with multiple rows of grinding teeth interspersed with grooves that shear against the lower jaw. Many rhynchosaur species can be distinguished from each other by the structure of their tooth plates. They had a fixed number of teeth, and similar to elephants, those that were further back in the jaws replaced teeth that were worn out as the animal grew in size and the teeth were worn out because of a diet of very tough plants. Rhynchosaur teeth were ankylothecodont, similar to the acrodonty of modern tuataras and some lizards, but differing in the presence of deep roots.
Rhynchosaurs first appeared during the Induan, the first stage of the Triassic, appearing shortly after the end-Permian mass extinction, as part of a major diversification of reptiles during this period. Like many animals of this time, they had a worldwide distribution, being found across Pangea, being especially common in the southern Gondwanan part of Pangaea, though with records also in Europe and North America. Over their evolution, rhynchosaurs saw a progressive increase in their body size. It has been suggested that rhynchosaurs went extinct near the end of the Carnian stage during the early Late Triassic as part of an end-Carnian extinction event.
Spielmann, Lucas and Hunt (2013) described three distal ends of humeri from the Bull Canyon Formation (Norian stage) in New Mexico. They interpreted these bones as belonging to rhynchosaurs within the species Otischalkia elderae; thus, they argued that these fossils indicate that rhynchosaur survival into the Norian. However, "Otischalkia" fossils were later reinterpreted as belonging to malerisaurine azendohsaurids. Rhynchosaurs apparently still survived into the Norian in Brazil, as Teyumbaita is known from the lower part of the Norian-age Caturrita Formation.
Historically, rhynchosaurs were considered to be closely related to Rhynchocephalia, the clade that includes the living tuatara and its extinct relatives. Today however the two groups are considered to be unrelated: rhynchosaurs are considered to be archosauromorphs (more closely related to modern crocodilians and birds), while rhynchocephalians are lepidosauromorphs (closer to lizards). Rhynchosaurs are considered members of the archosauromorph subclade Crocopoda.
Cladogram of Archosauromorpha after Schoch et al. 2025:
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Rhynchosauria
Rhynchosaurs are a group of extinct herbivorous Triassic archosauromorph reptiles, belonging to the order Rhynchosauria. Rhynchosaurs are distinguished by their triangular skulls and elongated, beak like premaxillary bones. Rhynchosaurs first appeared in the Early Triassic, reaching their broadest abundance and a global distribution during the Carnian stage of the Late Triassic, before dying out early in the succeeding Norian stage.
Rhynchosaurs were herbivores, and at times abundant (in some fossil localities accounting for 40 to 60% of specimens found), with stocky bodies and a powerful beak. Early primitive forms, like Mesosuchus and Howesia, were generally small, typically lizard-like in build, and had skulls rather similar to the early diapsid Youngina, except for the beak and a few other features. Later and more advanced genera grew to up to two meters in length. The hind feet were equipped with massive claws, presumably for digging up roots and tubers by backwards scratching of the hind limbs. Rhynchosaurs probably had a semi-erect posture (intermediate between most reptiles, which have a sprawling posture, and dinosaurs and mammals, which acquired an erect posture with a narrow stance).
The skulls of later rhynchosaurs were short, broad, and triangular, becoming much wider than long in the most advanced forms like Hyperodapedon. The toothless premaxilla bone, at the tip of the snout, extended outwards and downwards to form the upper beak. The broad skull had a deep cheek region which would have accommodated powerful jaw muscles. The lower jaw was also deep, and when the mouth was closed it clamped firmly into the maxilla (upper edge of the jaw), like the blade of a penknife closing into its handle. This scissors-like action would have enabled rhynchosaurs to cut up tough plant material.
The teeth were unusual; those in the maxilla and palate were modified into broad tooth plates, with multiple rows of grinding teeth interspersed with grooves that shear against the lower jaw. Many rhynchosaur species can be distinguished from each other by the structure of their tooth plates. They had a fixed number of teeth, and similar to elephants, those that were further back in the jaws replaced teeth that were worn out as the animal grew in size and the teeth were worn out because of a diet of very tough plants. Rhynchosaur teeth were ankylothecodont, similar to the acrodonty of modern tuataras and some lizards, but differing in the presence of deep roots.
Rhynchosaurs first appeared during the Induan, the first stage of the Triassic, appearing shortly after the end-Permian mass extinction, as part of a major diversification of reptiles during this period. Like many animals of this time, they had a worldwide distribution, being found across Pangea, being especially common in the southern Gondwanan part of Pangaea, though with records also in Europe and North America. Over their evolution, rhynchosaurs saw a progressive increase in their body size. It has been suggested that rhynchosaurs went extinct near the end of the Carnian stage during the early Late Triassic as part of an end-Carnian extinction event.
Spielmann, Lucas and Hunt (2013) described three distal ends of humeri from the Bull Canyon Formation (Norian stage) in New Mexico. They interpreted these bones as belonging to rhynchosaurs within the species Otischalkia elderae; thus, they argued that these fossils indicate that rhynchosaur survival into the Norian. However, "Otischalkia" fossils were later reinterpreted as belonging to malerisaurine azendohsaurids. Rhynchosaurs apparently still survived into the Norian in Brazil, as Teyumbaita is known from the lower part of the Norian-age Caturrita Formation.
Historically, rhynchosaurs were considered to be closely related to Rhynchocephalia, the clade that includes the living tuatara and its extinct relatives. Today however the two groups are considered to be unrelated: rhynchosaurs are considered to be archosauromorphs (more closely related to modern crocodilians and birds), while rhynchocephalians are lepidosauromorphs (closer to lizards). Rhynchosaurs are considered members of the archosauromorph subclade Crocopoda.
Cladogram of Archosauromorpha after Schoch et al. 2025:
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