Moa (order Dinornithiformes) are an extinct group of flightless birds formerly endemic to New Zealand. During the Late Pleistocene-Holocene, there were nine species, in six genera. The two largest species, Dinornis robustus and Dinornis novaezelandiae, reached about 3.6 metres (12 ft) in height with neck outstretched, and weighed about 230 kilograms (510 lb); the smallest, the bush moa (Anomalopteryx didiformis), was about the size of a turkey. Estimates of the moa population when Polynesians settled New Zealand circa 1300 C.E. range from 58,000 to 2.5 million. Moa are traditionally placed in the ratite group. Genetic studies have found that their closest relatives are the flighted South American tinamous, once considered a sister group to ratites. The nine species of moa were the only entirely wingless birds, lacking even vestigial wings, which all other ratites have. They were the largest terrestrial animals and dominant herbivores in New Zealand's forest, shrubland, and subalpine ecosystems until the arrival of the Māori, and were hunted only by Haast's eagle. Moa extinction occurred within 100 years of human settlement of New Zealand, primarily because of overhunting.
Etymology The word moa is a Polynesian term for domestic fowl. The name was not in common use among the Māori by the time of European contact, likely because the bird it described had been extinct for some time. Nevertheless, knowledge was passed down through traditional stories and proverbs, such as kua ngaro i te ngaro o te moa (lost as the moa is lost). The earliest written record of the name was by missionaries William Williams and William Colenso in January 1838; Colenso speculated that the birds may have resembled gigantic fowl. In 1912, Māori chief Urupeni Pūhara claimed that the moa's traditional name was te kura (the red bird). The North Island giant moa is also called kuranui.
Description
Moa skeletons were traditionally reconstructed in an upright position to create impressive height, but analysis of their vertebral articulations indicates that they probably carried their heads forward, in the manner of a kiwi. The spine was attached to the rear of the head rather than the base, indicating the horizontal alignment. This would have let them graze on low vegetation, while being able to lift their heads and browse trees when necessary. This has resulted in a reconsideration of the height of larger moa. However, Māori rock art depicts moa or moa-like birds with necks upright, indicating that moa were capable of assuming both neck postures.
No records survive of what sounds moa made, though some idea of their calls can be gained from fossil evidence. The trachea of moa were supported by many small rings of bone known as tracheal rings. These rings were preserved within some articulated skeletons, and shows that at least two moa genera (Euryapteryx and Emeus) exhibited tracheal elongation, where their trachea, up to 1 metre (3.3 feet) long, formed a large loop within the body cavity. They are the only ratites known to exhibit this feature, which is also present in several other bird groups, including swans, cranes, and guinea fowl. The feature is associated with deep resonant vocalisations that can travel long distances.
Feathers and soft tissues Several examples of moa remains have been found with soft tissues (muscle, skin, feathers) preserved through desiccation after the bird died at a dry site (for example, a cave with a constant dry breeze blowing through it); these specimens are a form of natural mummy. Most were found in the semiarid Central Otago region, the driest part of New Zealand, but others are known from outside the Central Otago region. These include:
Dried muscle on bones of a female Dinornis robustus found at Tiger Hill in the Manuherikia River Valley by gold miners in 1864 (currently held by Yorkshire Museum) Several bones of Emeus crassus with muscle attached, and a row of neck vertebrae with muscle, skin, and feathers collected from Earnscleugh Cave near the town of Alexandra in 1870 (currently held by the Otago Museum) An articulated foot of a male D. giganteus with skin and foot pads preserved, found in a crevice on the Knobby Range in 1874 (currently held by the Otago Museum) The type specimen of Megalapteryx didinus found near Queenstown in 1878 (currently held by Natural History Museum, London; see photograph of foot on this page) The lower leg of Pachyornis elephantopus, with skin and muscle, from the Hector Range in 1884; (currently held by the Zoology Department, Cambridge University) The complete feathered leg of a M. didinus from Old Man Range in 1894 (currently held by the Otago Museum) The head of a M. didinus found near Cromwell sometime before 1949 (currently held by Te Papa Tongarewa). A complete foot of M. didinus found in a cave on Mount Owen near Nelson in the 1980s (currently held by Te Papa Tongarewa) A skeleton of Anomalopteryx didiformis with muscle, skin, and feather bases collected from a cave near Te Anau in 1980.
In addition to these specimens, loose moa feathers have been collected from caves and rock shelters in the southern South Island, and based on these remains, some idea of the moa plumage has been achieved. The preserved leg of M. didinus from the Old Man Range reveals that this species was feathered right down to the foot. This is likely to have been an adaptation to living in high-altitude, snowy environments, and is also seen in the Darwin's rhea, which lives in a similar seasonally snowy habitat. Moa feathers are up to 23 cm (9 in) long, and a range of colours has been reported, including reddish-brown, white, yellowish, and purplish. Dark feathers with white or creamy tips have also been found, and indicate that some moa species may have had plumage with a speckled appearance.
Classification
Evolutionary relationships
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