The spotless crake (Zapornia tabuensis) is a species of bird in the rail family, Rallidae. It is widely distributed species occurring from the Philippines, New Guinea and Australia, across the southern Pacific Ocean to the Marquesas Islands and south to New Zealand.
Taxonomy
The spotless crake was formally described in 1789 by the German naturalist Johann Friedrich Gmelin in his revised and expanded edition of Carl Linnaeus's Systema Naturae. He placed it with the other crakes and rails in the genus Rallus and coined the binomial name Rallus tabuensis. Gmelin's account is taken from that of the "Tabuan rail" that had been described in 1785 by the English ornithologist John Latham in his book A General Synopsis of Birds. Latham's description was probably based on a plate painted by the German naturalist Georg Forster who had accompanied the British explorer James Cook on his second voyage to the Pacific Ocean. The genus name is an anagram of the genus Porzana that was introduced by the French ornithologist Louis-Pierre Vieillot. The specific epithet tabuensis is from Tongatapu, Tahiti, the type locality. The spotless crake was formerly placed in the genus Porzana but is assigned to the genus Zapornia that was introduced in 1816 by William Elford Leach. The species is monotypic: no subspecies are recognised.
Description
As an adult the spotless crake can reach a length of 17 – 20 cm; a wingspan of 26 – 29 cm; and can weigh between 40 – 50g. The head, and neck of the spotless crake is a bluish–grey slate colour. Some also have an occasional light grey or whitish patch on the chin, which can extend down the throat. The back, the outer wings, and inner wings have a dark reddish–brown which then fades into a dark blackish – brown on the tail feathers. The underside of the spotless crake is also a bluish–grey which then transitions to a blackish–grey on the underside of the tail feathers. Its bill is black, and its eyes are a deep red which contrast sharply with the head. The legs and feet are a reddish–pink colour. Spotless crake lack any obvious sexual dimorphism, making it difficult to distinguish between male and female.
The juvenile is similar to the adult, but its colouring is duller over the whole body, and is paler and browner than the mature crake. Its chin and throat have a white patch on it. The back is a dull brown, and the head and underside is a dull grey–brown. The eyes are a brownish-orange which then begin to turn red as it matures. The colour of the legs and feet can vary from an olive–brown, brownish–grey, or a brownish–flesh colour which also turn red as it matures.
The spotless crake has a variety of calls, although little is known about the meaning of each. Originally, seven separate calls of the spotless crake were detected, including a bubbling sound, a sharp, high pitched ‘pit-pit’, a ‘mook’ sound which varies in loudness and pitch, and a loud ‘purring’ call. The high-pitched ‘purr’ sound is believed to be its song. This call is made up of a rapid series of notes which are roughly 25 per second, making it its loudest call. More calls were detected at the time but since then only four have been described.
Distribution and habitat
The spotless crake is widely distributed throughout the south pacific including the Philippines, Moluccas, New Guinea, Melanesia, Australia, Tasmania, Norfolk Island, and south-west Polynesia including New Zealand, as well as Indonesia.
In New Zealand, the spotless crake, also known as pūweto, is distributed throughout the mainland. Numbers are few in the South Island with only a handful of isolated communities on the west coast, east coast, and Southland, New Zealand. The distribution in the North Island is spread far wider, but there are still few communities. Most sightings of spotless crake tend to be near the top of the North Island. Nationally important sites include: Awarua-Waituna wetland complex in Southland, New Zealand, Great Barrier Island, Kermadec Islands, Lake Wairarapa, Poor Knights Islands, Tiritiri Matangi Island, and Whangamarino wetland in Waikato. Other than on the mainland the spotless crake has been found on many offshore islands including: ‘Kermadec Islands, Manawatāwhi / Three Kings Islands, Poor Knights Island, and the Chatham Islands’. Fossils of the spotless crake from the Holocene period have also been found on the mainland, as well as the Chatham Islands. Because the spotless crake is rarely seen, it is hard to determine what the population size is, so currently population numbers are unknown in New Zealand.