Four pollen diagrams from Banks Island, Northwest Territories, provide the
first records of the postglacial vegetation of the region. Chronologies are
estimated from radiocarbon dates and by correlation of the exotic-pollen c
urves to data from the mainland. The pollen stratigraphies from all sites c
an be divided into three zones, where the middle zone, dating from 7000 to
2000 BP, corresponds to the warmest time. Although both the first and third
zones correspond to cooler periods, the vegetation of the earliest zone wa
s not identical to that of the latest, indicated by lower frequencies of ke
y pollen types such as those of Dryas and Saxifraga.