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The Māori settlement of New Zealand represents an end-point of a long chain of island-hopping voyages in the South Pacific.. Evidence from genetics, archaeology, linguistics, and physical anthropology indicates that the ancestry of Polynesian people stretches all the way back to indigenous peoples of Taiwan.
The best-known and most extensively studied Archaic site, at Wairau Bar in the South Island, [49] shows evidence of occupation from early-13th century to the early-15th century. [50] It is the only known New Zealand archaeological site containing the bones of people who were born elsewhere.
Polynesians are an ethnolinguistic group comprising closely related ethnic groups native to Polynesia, which encompasses the islands within the Polynesian Triangle in the Pacific Ocean. They trace their early prehistoric origins to Island Southeast Asia and are part of the larger Austronesian ethnolinguistic group, with an Urheimat in Taiwan.
Formerly known as Formosa, the island has been home to indigenous people for thousands of years, before the Dutch and Spanish briefly ruled parts of it in the 1600s.
This suggests heavy sea traffic took place between these islands and Taiwan at this time. [76] From around 5000 to 1500 BC, Taiwanese indigenous peoples started a seaborne migration to the island of Luzon in the Philippines, intermingling with the older Negrito populations of the islands. This was the beginning of the Austronesian expansion.
The Austronesian peoples refer to people sometimes referred to as Austronesian-speaking peoples, [44] and are meant to refer to a large group of peoples from places such as Taiwan, Maritime Southeast Asia, parts of Mainland Southeast Asia, Micronesia, coastal New Guinea, Island Melanesia, Polynesia, and Madagascar that speak languages that have been categorized by some as Austronesian languages.
Following World War II, political change came more slowly to the islands of Polynesia than to the other parts of overseas colonies of European powers. Although sovereignty was granted by royal proclamation to New Zealand as early as 1907, this did not fully come into effect until 1947.
In the Late Pleistocene, sea levels were about 140 metres (460 ft) lower than at present, exposing the floor of the shallow Taiwan Strait as a land bridge. [6] A concentration of vertebrate fossils has been found in the channel between the Penghu Islands and Taiwan, including a partial jawbone designated Penghu 1, apparently belonging to a previously unknown species of genus Homo, dated ...