The little penguin (Eudyptula minor) is a species of penguin from New Zealand. They are commonly known as little blue penguins or blue penguins owing to their slate-blue plumage and are also known by their Māori name kororā.
Penguins are a group of aquatic flightless birds. They live almost exclusively in the Southern Hemisphere: only one species, the Galápagos penguin, is found north of the Equator. Highly adapted for life in the water, penguins have countershaded dark and white plumage and flippers for swimming. Most penguins feed on krill, fish, squid and other forms of sea life which they catch with their bills and swallow it whole while swimming. A penguin has a spiny tongue and powerful jaws to grip slippery prey.
The Fiordland penguin, also known as the Fiordlandcrested penguin, is a crested penguin species endemic to New Zealand. It currently breeds along the south-western coasts of New Zealand's South Island as well as on Stewart Island/Rakiura and its outlying islands. Because it originally ranged beyond Fiordland, it is sometimes referred to as the New Zealand crested penguin.
The genus Eudyptula contains two species of penguin, found in southern Australia, Tasmania, and New Zealand. They are commonly known as the little penguin, little blue penguin, or, in Australia, fairy penguin. In the language of the Māori people of New Zealand, little penguins are known as kororā.
Korora oliveri, also referred to as Oliver's penguin, is a genus and species of extinct penguin from the Waitakian Stage of New Zealand. It was relatively small and slender, similar in size to one of the larger crested penguins. The penguin was described by Brian Marples in 1952 from fossil material he collected in the Hakataramea Valley, in the Canterbury region of the South Island. The genus name Korora is the Māori term for the extant little penguin. The specific epithet honours Walter Oliver (1883–1957) a former director of the Dominion Museum.
Archaeospheniscus is an extinct genus of large penguins. It currently contains three species, known from somewhat fragmentary remains. A. wimani, the smallest species, was found in Middle or Late Eocene strata of the La Meseta Formation on Seymour Island, Antarctica, whereas the other two, about the size of a modern emperor penguin, are known from bones recovered from the Late Oligocene Kokoamu Greensand Formation at Duntroon, New Zealand.
Archaeospheniscus lowei is the type species of the extinct penguin genus Archaeospheniscus. It stood approximately 85–115 cm high, between a modern king penguin and an emperor penguin in size. It is known from bones of a single individual and possibly some additional material such as the OM C.47.27 femur, all recovered from the Late Oligocene Kokoamu Greensand Formation at Duntroon, New Zealand.
Archaeospheniscus lopdelli was the largest species of the extinct penguin genus Archaeospheniscus, standing about 90–120 cm (35–47 in) high, or somewhat less than the extant emperor penguin. It is only known from bones of a single individual which was found in the Late Oligocene Kokoamu Greensand Formation at Duntroon, New Zealand. Bones apparently belonging to this species are now also known from the Late Eocene La Meseta Formation on Seymour Island, Antarctica.
Marples' penguin was a large species of the extinct penguin genus Palaeeudyptes.
The Chatham pigeon, also called the Chatham Island pigeon or parea, is a bird endemic to the Chatham Islands in New Zealand. Growing to 800g in weight and 55 cm in length, the Chatham Island pigeon is closely related to the kererū or New Zealand pigeon, the only other species in the genus Hemiphaga.
Manu antiquus is a species of extinct bird of uncertain affinities from the Oligocene of New Zealand. It was described by Brian Marples in 1946 from fossil material found near Duntroon, north Otago, in the South Island. Marples suggested that it might be an early albatross; subsequent researchers have speculated that it could be a pelagornithid; however, its affinities remain uncertain. The genus name Manu is Māori for “bird”; the specific epithet antiquus is Latin for “old” or “ancient”.
The South Island giant moa is an extinct moa from the genus Dinornis. The moa were ratites, flightless birds with a sternum without a keel. They also have a distinctive palate. The origin of these birds is becoming clearer as it is now believed that early ancestors of these birds were able to fly and flew to the southern areas in which they have been found.
The North Island snipe, also known as the little barrier snipe or tutukiwi, is an extinct species of bird in the sandpiper family, Scolopacidae, that was endemic to New Zealand.
Manuherikia is a genus of extinct species of ducks from the Miocene of New Zealand. It was described from fossil material of the Saint Bathans Fauna, in the lower Bannockburn Formation of the Manuherikia Group, found by the Manuherikia River in the Central Otago region of the South Island. The genus name comes from the name of the geological formation in which the fossils were found and, ultimately, from the Manuherikia River and its valley.
Dunstanetta johnstoneorum is a genus and species of extinct duck from the Miocene of New Zealand. It was described from fossil material collected from a Saint Bathans Fauna site on Home Hills Station, in the lower Bannockburn Formation of the Manuherikia Group, in the Manuherikia River valley in the Central Otago region of the South Island. The genus name refers to the Dunstan Range, the mountains of which overlook the fossil site. The specific epithet honours Ann and Euan Johnstone of Home Hills Station.
Marplesornis novaezealandiae, also referred to as Harris's penguin is a genus and species of extinct penguin from New Zealand. It was a relatively large penguin, about the same size as a king penguin. The age of the only known specimen is uncertain, being often mentioned as Late Pliocene in age. However, due to the complex geology of the collection site, its actual age is somewhere between Early Miocene and Late Pliocene.
Duntroonornis parvus, also referred to as the Duntroon penguin, is a genus and species of extinct penguin from the Late Oligocene of New Zealand. The penguin was relatively small, similar in size to the Fiordland crested penguin. It was described by Brian Marples in 1952 from fossil material collected near Duntroon, from the Kokoamu Greensand Formation, near the border between the Canterbury and Otago regions of the South Island. Fossils found at the Hakataramea Valley may also be referrable to this species. The genus name Duntroonornis means "Duntroon bird". The specific epithet is the Latin parvus ("small").
Tereingaornis moisleyi, also referred to as Moisley's penguin, is a genus and species of extinct penguin from the Middle Pliocene of New Zealand. It was slightly smaller than the extant Fiordland crested penguin. It was described by Ron Scarlett in 1983 from fossil material found by William Moisley near Te Reinga Falls on the Wairoa River, in the Hawke's Bay Region of the North Island. Another specimen was found later at Waihi Beach, Hawera, on the South Taranaki Bight. The genus name Tereingaornis combines the name of the type locality with the Greek ornis ("bird"); the specific epithet honours the discoverer of the fossil.
Pleistorallus flemingi, also referred to as Fleming's rail, is a genus and species of extinct bird in the rail family from the Middle Pleistocene of New Zealand. It was a large and stout rail about the same size as the extant takahē. It was described by Trevor Worthy in 1997 from fossil material found in coastal deposits near Marton, in the Rangitikei District of the North Island. The genus name Pleistorallus refers to the Pleistocene age of the fossils; the specific epithet honours Charles Fleming (1916–1987) for his contributions to New Zealand ornithology and palaeontology.
The South Island kōkako is a possibly extinct forest bird endemic to the South Island of New Zealand. Unlike its close relative, the North Island kōkako, it has largely orange wattles, with only a small patch of blue at the base, and was also known as the orange-wattled crow. The last accepted sighting in 2007 was the first considered genuine since 1967, although there have been several other unauthenticated reports.
