Rhynchocephalia

Rhynchocephalia (; ) is an order of lizard-like reptiles that includes only one living species, the tuatara (''Sphenodon punctatus'') of New Zealand. Despite its current lack of diversity, during the Mesozoic rhynchocephalians were a diverse group including a wide array of morphologically distinct forms. The oldest record of the group is dated to the Middle Triassic around 238 to 240 million years ago, and they had achieved a worldwide distribution by the Early Jurassic. Most rhynchocephalians belong to the group Sphenodontia ('wedge-teeth'). Their closest living relatives are lizards and snakes in the order Squamata, with the two orders being grouped together in the superorder Lepidosauria.

Many of the niches occupied by lizards today were held by sphenodontians during the Triassic and Jurassic, although lizard diversity began to overtake sphenodontian diversity in the Cretaceous, and they had disappeared almost entirely by the beginning of the Cenozoic. While the modern tuatara is primarily carnivorous, there were also sphenodontians with omnivorous ('' Opisthias''), herbivorous (Eilenodontinae), and durophagous ('' Oenosaurus'') lifestyles. There were even several successful groups of aquatic sphenodontians, such as pleurosaurs and '' Ankylosphenodon''.

History of discovery

Tuatara were originally classified as agamid lizards when they were first described by John Edward Gray in 1831. They remained misclassified until 1867, when Albert Günther of the British Museum noted features similar to birds, turtles, and crocodiles. He proposed the order Rhynchocephalia (meaning "beak head") for the tuatara and its fossil relatives. In 1925 Samuel Wendell Williston proposed the Sphenodontia to include only tuatara and their closest fossil relatives. ''Sphenodon'' is derived from Greek 'wedge' and 'tooth'. Many disparately related species were subsequently added to the Rhynchocephalia, resulting in what taxonomists call a " wastebasket taxon". These include the superficially similar (both in shape and name) but unrelated rhynchosaurs, which lived in the Triassic. These were resolved after use of computer based cladistics, which showed the core sphenodontian grouping to be monophyletic.

Classification and anatomy

Sphenodonts, and their sister group Squamata (which includes lizards, snakes and amphisbaenians), belong to the superorder Lepidosauria, the only surviving taxon within Lepidosauromorpha.

Squamates and sphenodontians have a number of shared traits ( synapomorphies), including fracture planes within the tail vertebrae allowing caudal autotomy (loss of the tail-tip when threatened), transverse cloacal slits, an opening in the pelvis known as the thyroid fenestra, the presence of extra ossification centres in the limb bone epiphyses, a knee joint where a lateral recess on the femur allows the articulation of the fibula, the development of a sexual segment of the kidney, and a number of traits of the feet bones, including a fused astralago- calcaneun and enlarged fourth distal tarsal, which creates a new joint, along with a hooked fifth metatarsal.

Like some squamates, the tuatara retains a parietal eye, which has been lost in the other groups of extant reptiles, the turtles and archosaurs. Rhynchocephalians are distinguished from squamates by a number of traits, including the retention of gastralia (rib-like bones present in the belly of the body, ancestrally present in tetrapods and also present in living crocodilians), a narrow quadrate bone, the temporal fenestra (an opening of the skull) is enclosed or partially enclosed by bone, the jugal bones in the temporal arch touch the squamosal bone posteriorly, and a large coronoid process is present on the lower jaw. The complete lower temporal bar of the tuatara, often considered a primitive feature, is actually a derived feature among sphenodontians, with the most primitive lepidosauromorphs and rhynchocephalians having an open lower temporal fenestra. Unlike squamates, but similar to the majority of birds, the tuatara lacks a penis. This is a secondary loss, as a penis or squamate-like hemipenes were probably present in the last common ancestor of rhynchocephalians and squamates.

The dentition of most rhynchocephalians is described as acrodont (the condition where the teeth are attached to the crest of the jaw bone, and lack roots), similar to those of acrodontan lizards like agamids. The term "acrodont" has also been used in reference to the absence of tooth replacement or the extent of bone growth around the teeth, causing terminological confusion. The teeth of living tuatara have no roots and are not replaced, and are extensively fused to the jaw bone. The teeth of ''Gephyrosaurus'' are pleurodont (teeth are weakly attached to the inner part of the mandible with no sockets, and replaced throughout life), like those of most squamates, and this is thought to be the ancestral condition of Lepidosauria. The most primitive sphenodontians have a combination of both pleurodont and acrodont teeth. Some rhyncocephalians differ from these conditions, with '' Ankylosphenodon'' having teeth that continue deeply into the jaw bone, and are fused to the bone at the base of the socket (ankylothecodont).

Rhynchocephalians possess palatal dentition (teeth present on the bones of the roof of the mouth). In most rhynchocephalians, the teeth present on the pterygoid bone are lost, but the lateral tooth row present on the palatine bones are enlarged, and orientated parallel to the teeth of the maxilla. During biting, the teeth of the dentary in the lower jaw slot between the maxillary and palatine tooth rows. This arrangement, which is unique among amniotes, permits three point bending of food items, and in combination with propalinal movement (back and forward motion of the lower jaw) allows for a shearing bite.

Internal systematics

While the grouping of Rhynchocephalia is well supported, the relationships of many taxa to each other are uncertain, varying substantially between studies. In modern cladistics, the clade Sphenodontia includes all rhynchocephalians other than '' Gephyrosaurus'' (as well as some other related genera) which has been found to be more closely related to squamates in some analyses. In 2018, two major clades within Sphenodontia were defined, the infraorder Eusphenodontia which is defined by the least inclusive clade containing '' Polysphenodon, Clevosaurus hudsoni'' and ''Sphenodon'', which is supported by the presence of three synapomorphies, including the presence of clearly visible wear facets on the teeth of the dentary or maxilla, the premaxillary teeth are merged into a chisel like structure, and the palatine teeth are reduced to a single tooth row, with the presence of an additional isolated tooth. The unranked clade Neosphenodontia (previously informally referred to as the "eupropalinals", in reference to the back and forward motion in the mouth during mastication), is defined as the most inclusive clade containing ''Sphenodon'' but not ''Clevosaurus hudsoni,'' which is supported by the presence of six synapomorphies, including the increased relative length of the antorbital region of the skull (the part of the skull forward of the eye socket), reaching 1/4 to 1/3 of the total skull length, the posterior (hind) edge of the parietal bone is only slightly curved inward, the parietal foramen is found at the same level or forward of the anterior border of the supratemporal fenestra (an opening of the skull), the palatine teeth are further reduced from the condition in eusphenodontians to a single lateral tooth row, the number of pterygoid tooth rows are reduced to one or none, and the posterior border of the ischium is characterised by a distinctive process.

The family Sphenodontidae has been used to include the tuatara and its closest relatives within Rhynchocephalia. However the grouping has lacked a formal definition, with the included taxa varying substantially between analyses. The closest relatives of the tuatara are placed in the clade Sphenodontinae, which are characterised by a completely closed termporal bar.

Paleobiology

Rhynchocephalians were once considered to be a morphologically conservative group with little diversity. However, discoveries in recent decades have disputed this, finding a wide array of diversity within the clade. Early rhynchocephalians possess small ovoid teeth designed for piercing, and were probably insectivores. Amongst the most distinct rhynchocephalians are the pleurosaurs, known from the Jurassic of Europe, which were adapted for marine life, with elongated snake-like bodies with reduced limbs, with the specialised Late Jurassic genus '' Pleurosaurus'' having an elongated triangular skull highly modified from those of other rhynchocephalians. Several other lineages of rhyncocephalians have been suggested to have had semi-aquatic habits. Eilenodontines are thought to have been herbivorous, with batteries of wide teeth with thick enamel used to process plant material. '' Oenosaurus'' and '' Sapheosaurus'' from the Late Jurassic of Europe possess broad tooth plates unique amongst tetrapods, and are thought to have been durophagous, with the tooth plates being used to crush hard shelled organisms.

Evolutionary history

Rhynchocephalia is estimated to have diverged from Squamata between the Middle Permian and earliest Triassic, between 270 and 252 million years ago. The oldest known remains of rhynchocephalians are indeterminate jaw fragments from the Erfurt Formation near Vellberg in Southern Germany, dating to the Ladinian stage of the Middle Triassic, around 238-240 million years old. Rhynchocephalians reached a worldwide distribution across Pangaea by the end of the Triassic, with the Late Triassic- Early Jurassic genus '' Clevosaurus'' having 10 species across Asia, Africa, Europe, North and South America. The earliest rhynchocephalians were small animals, but by the Late Triassic the group had evolved a wide range of body sizes. During the Jurassic rhynchocephalians reached their apex of morphological diversity, including specialised herbivorous and aquatic forms. The only record of Rhynchocephalians from Asia are indeterminate remains of ''Clevosaurus'' from the Early Jurassic ( Sinemurian) aged Lufeng Formation of Yunnan, China. Rhynchocephalians are noticeably absent from younger localities in the region, despite the presence of favourable preservation conditions.

Rhynchocephalians disappeared from North America and Europe after the Early Cretaceous, and were absent from North Africa and northern South America by the early Late Cretaceous. The cause of the decline of Rhynchocephalia remains unclear, but has often been suggested to be due to competition with advanced lizards and mammals. They appear to have remained diverse in high-latitude southern South America during the Late Cretaceous, where lizards remained rare, with their remains outnumbering terrestrial lizards by a factor of 200. The youngest known remains of rhynchocephalians outside of New Zealand are those of ''Kawasphenodon peligrensis'' from the early Paleocene (Danian) of Patagonia, shortly after the Cretaceous–Paleogene extinction event. Indeterminate sphenodontine jaw fragments bearing teeth are known from the early Miocene (19-16 million years ago) St Bathans fauna, New Zealand, that are indistinguishable from those of the living tuatara. It is unlikely that the ancestors of the tuatara arrived in New Zealand via oceanic dispersal, and it is thought that they were already present in New Zealand when it separated from Antarctica between 80 and 66 million years ago.

Gallery

Phylogeny

The following is a cladogram of Rhynchocephalia after Rauhut et al., 2012.

References

Further reading

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External links

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{{Taxonbar, from=Q15099738

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Taxa named by Albert Günther
Tetrapod orders
Extant Middle Triassic first appearances
Ladinian first appearances
Middle Triassic taxonomic orders
Late Triassic taxonomic orders
Early Jurassic taxonomic orders
Middle Jurassic taxonomic orders
Late Jurassic taxonomic orders
Early Cretaceous taxonomic orders
Late Cretaceous taxonomic orders
Paleocene taxonomic orders
Eocene taxonomic orders
Oligocene taxonomic orders
Miocene taxonomic orders
Pliocene taxonomic orders
Pleistocene taxonomic orders
Holocene taxonomic orders