A 3.5m section of organic sediment was obtained from a karstic pond on
a hill in the centre of the Baliem Valley, one of the major settled i
ntermontane highland areas of New Guinea. The material spans two time
periods each of approximately 2 millennia, one from about 2000 BP to t
he present and the other from 33,500 to 31,500 BP. The pollen analysis
of the earlier section showed that it formed when the valley was fore
sted by Nothofagus forest, but a carbonized particle input was consist
ently present after about 32,500 years ago. The recent section covers
a period when the hill was totally cleared except for grassland and so
me open shrubby regrowth. The early burning and associated clearances
are tentatively ascribed to a human origin. Fire is associated with sl
ope erosion on the hill at 28,000 BP which supports the hypothesis of
long term human settlement in the area.