Abstract
During the mid- and late Holocene, the southern portion of the peninsula supported a rich deciduous forest, dominated by Acer saccharum and Fagus grandifolia, while the northern portion was dominated by a forest with a much higher proportion of conifers. The two sites are compared numerically with a site on Manitoulin Island. Despite similar bedrock, soils, climate, and topography, 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. -from Author
| Original language | English |
|---|---|
| Pages (from-to) | 6-18 |
| Number of pages | 13 |
| Journal | Canadian Journal of Botany |
| Volume | 70 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 1 Jan 1992 |
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SDG 13 Climate Action
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