The largest island of Oceania, New Guinea (800,000 square kilometres) was joined to Australia in periods of Pleistocene low sea-level, and was probably first settled by early Australoids at the same time as its larger neighbour (see Kosipe). New Guinea archaeology is best considered under two headings: the Highlands, totally PAPUAN-speaking, and the coasts, mixed Papuan and Austronesian. For the Highland prehistoric sequence in general (totally aceramic), see Kafiavana, Kiowa, Kosipe. For horticultural origins early in the Holocene, see Kuk. Stone mortars and pestles, many of elaborate shape, are also found in the Highlands, but their significance is still uncertain. The New Guinea coasts only have sequences back to 3000-2000 years ago so far (earlier sites probably being drowned by rising sea levels), and the best reported are from Collingwood Bay and south coastal Papua (both with pottery). Some coastal groups had developed elaborate trading networks by the time of European contact (see Motupore). See also Lake Sentani, Papuan, Sahul, sugar cane.
The Macmillan dictionary of archaeology, Ruth D. Whitehouse, 1983Copied