Abstract
Three new Holocene pollen percentage and accumulation rate diagrams for S Ontario are presented. In the earliest Holocene, the forests were dominated by Picea, which was replaced by first Pinus banksiana - resinosa and then Pinus strobus. In extreme S Ontario, Pinus strobus was replaced by Acer saccharum and Fagus grandifolia, but in the area east of Georgian Bay, Tsuga canadensis became the dominant, and near Mattawa, Betula (probably lutea). Late Holocene stability of forests is considered to be a function of the lack of taxa better able to compete than those already present. -from Author
Original language | English |
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Pages (from-to) | 1792-1801 |
Number of pages | 10 |
Journal | Canadian Journal of Botany |
Volume | 65 |
Issue number | 9 |
DOIs | |
Publication status | Published - 1 Jan 1987 |
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Dive into the research topics of 'Holocene history of forest trees in southern Ontario.'. Together they form a unique fingerprint.Datasets
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Lac Bastien pollen dataset
Bennett, K. D. (Contributor), Neotoma Paleoecology Database, 1 Jan 2017
DOI: 10.21233/n3pq5c
Dataset
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Nutt Lake pollen dataset
Bennett, K. D. (Contributor), Neotoma Paleoecology Database, 1 Jan 2017
DOI: 10.21233/n39m01
Dataset
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Hams Lake pollen dataset
Bennett, K. D. (Contributor), Neotoma Paleoecology Database, 1 Jan 2017
DOI: 10.21233/n39k8q
Dataset