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Through Endemism and Species

The single extant species of tuatara is the only surviving member of its order, which was highly diverse during the Mesozoic era. Rhynchocephalians first appeared in the fossil record during the Middle Triassic, around 244–241.5 million years ago, and reached worldwide distribution and peak diversity during the Jurassic, when they represented the world's dominant group of small reptiles. Rhynchocephalians declined during the Cretaceous, with their youngest records outside New Zealand dating to the Paleocene. Their closest living relatives are squamates (lizards and snakes). Tuatara are of interest for studying the evolution of reptiles.

Tuatara are greenish brown and grey, and measure up to 80 cm (31 in) from head to tail-tip and weigh up to 1.3 kg (2.9 lb) with a spiny crest along the back, especially pronounced in males. They have a second row of upper teeth on the roof of the mouth. They are able to hear, although no external ear is present, and have a number of unusual features in their skeleton compared to lizards, including gastralia in the belly, proatlas bones in the neck, and a completely fused temporal bar at the back of the skull.

Tuatara are sometimes referred to as "living fossils". This term is currently deprecated among paleontologists and evolutionary biologists. Although tuatara have preserved the morphological characteristics of their Mesozoic ancestors (240–230 million years ago), there is no evidence of a continuous fossil record to support the idea that the species has survived unchanged since that time.

The tuatara has been protected by law since 1895. Tuatara, like many of New Zealand's native animals, are threatened by habitat loss and introduced predators, such as the Polynesian rat (Rattus exulans). Tuatara were extinct on the mainland, with the remaining populations confined to 32 offshore islands, until the first North Island release into the heavily fenced and monitored Karori Wildlife Sanctuary (now named "Zealandia") in 2005. During routine maintenance work at Zealandia in late 2008, a tuatara nest was uncovered, with a hatchling found the following autumn. This is thought to be the first case of tuatara successfully breeding in the wild on New Zealand's North Island in over 200 years.

Taxonomy and evolution

Relationships of the tuatara to other living reptiles and birds, after Simões et al. 2022

Tuatara, along with other now-extinct members of the order Rhynchocephalia, belong to the superorder Lepidosauria, as do the order Squamata, which includes lizards and snakes. Squamates and tuatara both show caudal autotomy (loss of the tail-tip when threatened), and have transverse cloacal slits.

Tuatara were originally classified as lizards in 1831 when the British Museum received a skull. John Edward Gray used the name Sphenodon to describe the skull; this remains the current scientific name for the genus. Sphenodon is derived from the Greek for "wedge" (σφήν, σφηνός/sphenos) and "tooth" (ὀδούς, ὀδόντος/odontos). In 1842, Gray described a member of the species as Hatteria punctata, not realising that it and the skull he received in 1831 were both tuatara.

The genus remained misclassified as a lizard until 1867, when Albert C. L. G. 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. Since 1869, Sphenodon punctatus (or the variation Sphenodon punctatum in some earlier sources) has been used as the scientific name for the species.

At one point, many disparate species were incorrectly referred to the Rhynchocephalia, resulting in what taxonomists call a "wastebasket taxon". Williston in 1925 proposed the Sphenodontia to include only tuatara and their closest fossil relatives. However, Rhynchocephalia is the older name and in widespread use today. Many scholars use Sphenodontia as a subset of Rhynchocephalia, including almost all members of Rhynchocephalia, apart from the most primitive representatives of the group.

The earliest rhynchocephalian, Agriodontosaurus, is known from the Middle Triassic (Anisian) of England, around 244 to 241.5 million years ago. During the Late Triassic, rhynchocephalians greatly diversified, going on to become the world's dominant group of small reptiles during the Jurassic period, when the group was represented by a diversity of forms, including the aquatic pleurosaurs and the herbivorous eilenodontines. The earliest members of Sphenodontinae, the clade which includes the tuatara, are known from the Early Jurassic of North America around 190 million years ago. The earliest sphenodontines are already very morphologically similar to the modern tuatara. Rhynchocephalians declined during the Cretaceous period, possibly due to competition with mammals and lizards, with their youngest record outside of New Zealand being of Kawasphenodon (which may be a sphenodontine), known from the early Paleocene (c. 66–60 million years ago) of southern Patagonia in South America.

Fossil material that can be referred to as sphenodontine is known from the early Miocene (c. 19–16 million years ago) Saint Bathans fauna of Otago in the South Island of New Zealand. Whether these specimens are referable to the genus Sphenodon proper is not entirely clear due to their incomplete nature, but they are likely to be from a taxon that is closely related to tuatara. Therefore, the ancestors of the tuatara were likely already present in New Zealand prior to its separation from Antarctica around 82–60 million years ago.

Cladogram of the position of the tuatara within Sphenodontia, after Simoes et al., 2022:

Species

While there is currently considered to be only one living species of tuatara, two species were previously identified: Sphenodon punctatus, or northern tuatara, and the much rarer Sphenodon guntheri, or Brothers Island tuatara, which is confined to North Brother Island in Cook Strait. The specific name punctatus is Latin for "spotted", and guntheri refers to German-born British herpetologist Albert Günther. A 2009 paper re-examined the genetic bases used to distinguish the two supposed species of tuatara, and concluded they represent only geographic variants, and only one species should be recognised. Consequently, the northern tuatara was re-classified as Sphenodon punctatus punctatus and the Brothers Island tuatara as Sphenodon punctatus guntheri. The Brothers Island tuatara has olive brown skin with yellowish patches, while the colour of the northern tuatara ranges from olive green through grey to dark pink or brick red, often mottled, and always with white spots. In addition, the Brothers Island tuatara is considerably smaller. However, individuals from Brothers Island could not be distinguished from other modern and fossil samples on the basis of jaw morphology.

An extinct species of Sphenodon was identified in November 1885 by William Colenso, who was sent an incomplete subfossil specimen from a local coal mine. Colenso named the new species S. diversum. Fawcett and Smith (1970) consider it a synonym to the subspecies, based on a lack of distinction.

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