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Tikopia

Tikopia, a Polynesian community near the eastern border of the Solomon Islands, is arguably the most thoroughly documented small-scale society in the ethnographic record. That documentation exists primarily as a result of investigations by Sir Raymond Firth in 1928–29, 1952,1966, and 1973. Based on those four field visits, he published nine full-length books and countless articles. In addition to Firth's path-breaking research, studies of varying length have been conducted by social anthropologists James Spillius, Torben Monberg, Eric Larson, and Judith Macdonald; ethnobotanist Douglas Yen; and archaeologist Patrick Kirch.

Tikopia is a “Polynesian outlier,” meaning that its people are linguistically, culturally, and physically Polynesian, although their home lies outside of what we normally think of as the Polynesian heartland—a vast triangle bounded by Hawai'i in the north,Rapanui (Easter Island) in the east, and Aotearoa (New Zealand) in the west. It is located at 12° 18' S by 168° 48' E. Tikopia's climate is tropical. Its yearly calendar is divided into two seasons, generally termed the “trade-wind” and “monsoon” seasons (in Tikopian, te tonga and te raki, respectively). The trade-wind season, running from somewhere in April to October, is characterized by strong breezes blowing constantly from the southeast. It is relatively cool and tends to be the drier of the two seasons. The monsoon season is characterized by unstable weather. Blazing sun is interspersed with torrential rains, and extended periods of calm are interrupted by violent storms.

The island is approximately three miles from northeast to southwest and1.5 miles from southeast to northwest. It is of volcanic origin and rises to a maximum altitude of about 1,200 feet. Tikopia's nearest neighbor is Anuta, 70 miles to the northeast, which it resembles in language and culture. To the west, its nearest neighbors are the Melanesian islands of Vanikoro, Utupua, and Ndenö, the Polynesian island of Taumako, and the Reef Islands with their mixture of Polynesian and non-Austronesian speakers. Tikopia's population at the time of Firth's initial study was around 1,270. Owing to substantial out-migration since the 1950s, the current resident population is only slightly larger, but there are now large Tikopian settlements on Vanikoro, Makira, Guadalcanal, and in the Russell Islands.

Prehistory

According to oral traditions, Tikopia was pulled up from the ocean floor by the demigod Metikitiki. The original occupants, the Atua i Raropuka (the Deity of Raropuka) and the Atua Fafine (the Female Deity), introduced the prototypical male and female economic activities: preparing sennit cord and plaiting pandanus-leaf mats. Several of the current descent lines claim autochthonous origin; others are said to have arrived from such diverse locales as Tonga,Pukapuka, Samoa, ‘Uvea, Rotuma, Ontong Java, Motulava, and Anuta. Tikopians speak a Nuclear Polynesian language, related to Samoan and Tuvaluan.

Kirch's archaeological investigations indicate a period of continuous habitation spanning almost three thousand years, with tenuous suggestions of sporadic visits dating back close to another thousand. Kirch and Yen divide the island's cultural history into four periods, each typified by a distinctive artifactual assemblage. The earliest, which they term the “Kiki Phase,” is characterized by Lapitoid ceramic ware, and it lasted from about 900 to 100 BC. The Kiki Phase gave way rather abruptly to the “Sinapupu Phase,” characterized by incised Mangaasi-style pottery, apparently imported from northern Vanuatu. The Sinapupu Phase lasted to perhaps the 15th century AD and gradually gave way to the “Tuakamali Phase.” The latter period is distinguished by a characteristically Polynesian artifactual assemblage and complete disappearance of ceramic ware. European contact began with Quiros's visit in AD 1606. Kirch and Yen use AD 1800 as the date marking the end of the Tuakamali and the inception of the “Historic Phase.”

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