Definitive evidence for the onset of monsoon moisture in northern Australia
following the and phase of the Last Glacial Maximum has been elusive, in l
arge part due to the lack of long, continuous sediment records. Here we rep
ort new evidence from two separate drainage basins in the Kimberley region
of monsoonal northwestern Australia. At both sites, radiocarbon ages on (ba
sal) biogenic materials in flood deposits indicate stream flow, as high or
higher than maximum historic levels, began about 14 cal ka BP. These result
s suggest that the Australian summer monsoon was fully active several mille
nnia earlier than previously expected. The early onset of the monsoon and t
he widespread evidence for diminished monsoon activity in the late Holocene
cannot be reconciled with primary forcing of the Australian monsoon by cha
nges in low-latitude summer insolation over Australia. (C) 2001 Elsevier Sc
ience Ltd and INQUA. All rights reserved.