Two new pollen sequences from the Bruce Peninsula. southern Ontario. d
emonstrate the Holocene history of forests in the area. During the mid
- and late Holocene, the southern portion of the peninsula supported a
rich deciduous forest, dominated by Acer saccharum and Fagus grandifo
lia, while the northern portion was dominated by a forest with a much
higher proportion of conifers. These two sites are compared numericall
y with a third site, on Manitoulin Island, by means of principal compo
nents analysis. Despite similar bedrock, soils, climate, and topograph
y, the three pollen sequences show a remarkable divergence of Holocene
forest history. The role of historical factors in determining forest
composition may be much greater than previously appreciated. This stud
y emphasises the need to understand the magnitude of variation between
pollen sequences within uniform terrain before ascribing the differen
ces in pollen sequences from contrasting environments (because of clim
ate, soils or topography) to the factors causing the obvious contrast.