List Of Oceanian Animals Extinct In The Holocene
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List Of Oceanian Animals Extinct In The Holocene
This list of Oceanian animals extinct in the Holocene features animals known to have become extinct in the last 12,000 years on the Oceanian continent, with the exclusion of Australia-New Guinea, New Zealand, and Hawaii, which are listed in separate articles. Many extinction dates are unknown due to a lack of relevant information. Mammals Birds Undated Prehistoric Recent Local Reptiles Amphibians Insects Molluscs Undated Recent Local See also * List of extinct animals * List of extinct animals of Australia * List of extinct animals of the Hawaiian Islands * List of extinct animals of New Zealand * List of extinct birds * Extinct in the wild * Lazarus taxon * U.S. Fish and Wildlife Service * IUCN Red List of Threatened Species Notes References {{Extinct Animals by Regions , state=autocollapsed Oceania Oceania (, , ) is a region, geographical region that includes Australasia, Melanesia, Micronesia, and Polynesia. Spanning the Eastern ...
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Oceania UN Geoscheme Regions
Oceania (, , ) is a geographical region that includes Australasia, Melanesia, Micronesia, and Polynesia. Spanning the Eastern and Western hemispheres, Oceania is estimated to have a land area of and a population of around 44.5 million as of 2021. When compared with (and sometimes described as being one of) the continents, the region of Oceania is the smallest in land area and the second least populated after Antarctica. Its major population centres are Sydney, Melbourne, Brisbane, Perth, Auckland, Adelaide, Honolulu, and Christchurch. Oceania has a diverse mix of economies from the highly developed and globally competitive financial markets of Australia, French Polynesia, Hawaii, New Caledonia, and New Zealand, which rank high in quality of life and Human Development Index, to the much less developed economies of Kiribati, Papua New Guinea, Tuvalu, Vanuatu, and Western New Guinea, while also including medium-sized economies of Pacific islands such as Fiji, Palau, and Tong ...
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New Caledonia
) , anthem = "" , image_map = New Caledonia on the globe (small islands magnified) (Polynesia centered).svg , map_alt = Location of New Caledonia , map_caption = Location of New Caledonia , mapsize = 290px , subdivision_type = Sovereign state , subdivision_name = , established_title = Annexed by France , established_date = 24 September 1853 , established_title2 = Overseas territory , established_date2 = 1946 , established_title3 = Nouméa Accord , established_date3 = 5 May 1998 , official_languages = French , regional_languages = , capital = Nouméa , coordinates = , largest_city = capital , demonym = New Caledonian , government_type = Devolved parliamentary dependency , leader_title1 = President of France , leader_name1 = Emmanuel Macron , leader_title2 = President of the Government , leader_name2 = Louis Mapou , leader_title3 = President of the Congress , leader_name3 = Roch Wamytan , leader_title4 = High Commissioner , leader_name4 = Patrice ...
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Powerful Goshawk
The powerful goshawk (''Accipiter efficax''), also referred to as the greater New Caledonian goshawk, is an extinct species of bird of prey in the family Accipitridae. It was endemic to the island of New Caledonia in Melanesia in the southwest Pacific region. It was described from subfossil bones found at the Pindai Caves paleontological site on the west coast of Grande Terre. The Latin specific epithet In taxonomy, binomial nomenclature ("two-term naming system"), also called nomenclature ("two-name naming system") or binary nomenclature, is a formal system of naming species of living things by giving each a name composed of two parts, bot ... ''efficax'' means "powerful". References {{Taxonbar, from=Q339143 Accipiter Extinct birds of New Caledonia Holocene extinctions Birds described in 1989 Taxa named by Jean-Christophe Balouet Late Quaternary prehistoric birds ...
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Mangaia Crake
The Mangaia crake (''Porzana rua'') is an extinct species of flightless bird in the rail family, Rallidae. History The crake was described in 1986 from subfossil bones of late Holocene age found in caves on the island of Mangaia, in the southern Cook Islands of East Polynesia Polynesia () "many" and νῆσος () "island"), to, Polinisia; mi, Porinihia; haw, Polenekia; fj, Polinisia; sm, Polenisia; rar, Porinetia; ty, Pōrīnetia; tvl, Polenisia; tkl, Polenihia (, ) is a subregion of Oceania, made up of .... The cause of its extinction is ascribed to a combination of predation and habitat alteration following human settlement of the island and the introduction of exotic mammals. See also * List of birds of the Cook Islands References Mangaia crake Birds of Mangaia Extinct flightless birds Extinct birds of Oceania Late Quaternary prehistoric birds Holocene extinctions Fossil taxa described in 1986 Mangaia crake {{paleo-bird-stub ...
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Lapitiguana Impensa
''Lapitiguana impensa'' is an extinct giant (1.5 m long) iguanid from Fiji. It probably became extinct following the human colonization of Fiji 3000 years ago. All extant Fijian iguanas are in the genus ''Brachylophus'', together with an extinct species from Tonga. The closest living relatives of the Polynesia Polynesia () "many" and νῆσος () "island"), to, Polinisia; mi, Porinihia; haw, Polenekia; fj, Polinisia; sm, Polenisia; rar, Porinetia; ty, Pōrīnetia; tvl, Polenisia; tkl, Polenihia (, ) is a subregion of Oceania, made up of ...n iguanas are found in the Americas. See also *'' Brachylophus gibbonsi'' *'' Pumilia novaceki'' References External linksFossil remains of the giant iguana ''Lapitiguana impensa''Lapitiguana impensa; holotype
...
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Viti Levu Giant Pigeon
The Viti Levu giant pigeon or Fiji giant ground pigeon (''Natunaornis gigoura'') is an extinct flightless pigeon of Viti Levu, the largest island in Fiji. It was only slightly smaller than the dodo (''Raphus cucullatus'') and Rodrigues solitaire (''Pezophaps solitaria'') and is the first giant, flightless pigeon to be discovered on a Pacific island. Remains of this species were discovered in Quaternary (probably Holocene) Cave deposits in October 1998 and November 1999. Its first description was published in 2001. The holotype is in the collection of the Museum of New Zealand Te Papa Tongarewa. It is known from the holotype tarsometatarsus and paratypes including various parts of the wings and legs. No parts of the skull are known apart from a possible referred premaxilla (MNZ S37306). The generic name "''Natunaornis''" is named after Natuna, the oldest chief of the Volivoli people in the Sigatoka Valley, wherein the fossil bones of the type species were first found. The ...
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Mangaia
Mangaia (traditionally known as A'ua'u Enua, which means ''terraced'') is the most southerly of the Cook Islands and the second largest, after Rarotonga. It is a roughly circular island, with an area of , from Rarotonga. Originally heavily populated, Mangaia's population has dropped by 75% in the last 50 years. Geography Originally known as ''A'ua'u'' or ''A'ua'u Enua'' ("terraced"), the island was named Mangaia (or ''Mangaianui-Neneva'', "Mangaia monstrously-great") by Tamaeu, who came to the island from Aitutaki in 1775. Geologists estimate the island is at least 18 million years old. It rises 4750 m (15,600 ft) above the ocean floor and has a land area of 51.8 km2. Surrounded by a fringing coral reef, like many of the southern Cook Islands, it is surrounded by a high ring of cliffs of fossil coral 60 m (200 ft) high, known as the makatea. The inner rim of the ''makatea'' forms a steep cliff, surrounding swamps and a central volcanic plateau. The interi ...
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Mangaia Rail
The Mangaia rail (''Gallirallus ripleyi'') is an extinction, extinct species of flightless bird in the rail family (biology), family, Rallidae. History The rail was described in 1986 from subfossil bones of late Holocene age found in caves on the island of Mangaia, in the southern Cook Islands of West Polynesia. The cause of its extinction is ascribed to a combination of predation and habitat alteration following human settlement of the island and the introduction of exotic mammals. See also * List of birds of the Cook Islands References

Gallirallus, Mangaia rail Birds of Mangaia Extinct flightless birds Extinct birds of Oceania Late Quaternary prehistoric birds Holocene extinctions Fossil taxa described in 1986 Birds described in 1986, Mangaia rail {{paleo-bird-stub ...
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Niue
Niue (, ; niu, Niuē) is an island country in the South Pacific Ocean, northeast of New Zealand. Niue's land area is about and its population, predominantly Polynesian, was about 1,600 in 2016. Niue is located in a triangle between Tonga, Samoa, and the Cook Islands. It is 604 kilometres northeast of Tonga. The island is commonly referred to as "The Rock", which comes from the traditional name "Rock of Polynesia". Niue is one of the world's largest coral islands. The terrain of the island has two noticeable levels. The higher level is made up of a limestone cliff running along the coast, with a plateau in the centre of the island reaching approximately 60 metres (200 feet) above sea level. The lower level is a coastal terrace approximately 0.5 km (0.3 miles) wide and about 25–27 metres (80–90 feet) high, which slopes down and meets the sea in small cliffs. A coral reef surrounds the island, with the only major break in the reef being in the central western c ...
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Niue Rail
The Niue rail (''Gallirallus huiatua'') is an extinct species of flightless bird in the Rallidae, or rail family. History The rail was described in 2000 from subfossil bones collected in January 1995 by paleozoologist Trevor Worthy at the Anakuli cave site in Hakupu village, on the island of Niue in West Polynesia. The age range of about 5300 to 3600 year BP for fossil material collected from the site predates human settlement of the island.(subscription required) Etymology The specific epithet comes from the Niuean words ''hui'' (bones) and ''atua'' (of the dead). See also * List of birds of Niue There are 57 species of birds that have been recorded on Niue, of which one has been introduced by humans.Watling, Dick (2001) ''A Guide to the Birds of Fiji & Western Polynesia'', Environmental Consultants (Fiji), Suva. Two species are globall ... References Gallirallus Extinct flightless birds Birds of Niue Late Quaternary prehistoric birds Holocene extinctions Fo ...
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New Caledonian Snipe
The New Caledonian snipe (''Coenocorypha neocaledonica'') is an extinct species of austral snipe, described from late Holocene cave deposits on the French island of New Caledonia in the western Pacific Ocean. The specific epithet is a latinisation of the name of its island home. Description Although austral snipe are small birds, the endemic New Caledonian form was larger than all its congeners, with the exception of the Viti Levu snipe The Viti Levu snipe (''Coenocorypha miratropica'') is an extinct species of austral snipe endemic to Fiji. A species of the mostly New Zealand genus ''Coenocorypha The austral snipes, also known as the New Zealand snipes or tutukiwi, are a g ... (''C. miratropica''). Examination of its wing bones suggest that it was a relatively strong flier. Extinction The species became extinct within about 1000 years of human settlement of the island, probably as a result of predation by human introduced rats. References Fossil taxa descri ...
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Viti Levu
Viti Levu (pronounced ) is the largest island in the Republic of Fiji. It is the site of the nation's capital, Suva, and home to a large majority of Fiji's population. Geology Fiji lies in a tectonically complex area between the Australian Plate and the Pacific Plate. The Fiji Platform lies in a zone bordered by active extension fault lines, around which most of the shallow earthquakes in the area have been centred. These fault lines are: the Fiji Fracture Zone (FFZ) to the north; the 176° Extension Zone (176°E EZ) to the west; and the Hunter Fracture Zone (HFZ) and Lau Ridge to the east. The oldest rocks on the island are those formed during the Eocene and Lower Miocene epochs that belong to the Wainimala group. The lower portion of the group is made up of volcanic flows and volcanoclastics, which grade from basalt to trachyte and rhyolite. Geographically, this group is found south of Nadi, including on the peaks of Koromba (at 3528 feet high) and Natambumgguto (at 1242 ...
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