K. Gajewski et M. Frappier, A holocene lacustrine record of environmental change in northeastern Prince of Wales Island, Nunavut, Canada, BOREAS, 30(4), 2001, pp. 285-289
A core from Prince of Wales Island in the central Canadian Arctic was analy
sed for pollen and sediment characteristics. From 9200 yr BP to 7000 yr BP,
the landscape supported a pioneer vegetation under cold conditions, with r
elatively high sediment input to the lake. Between 7000 and 4000 yr BP ther
e was a period of high pollen concentrations, more abundant Cyperaceae and
Dryas an the landscape and finer sediment input. In the last 4000 years, cl
imate cooling is indicated.