Late Holocene deforestation of a tree line site: estimation of pre‐fire vegetation composition and black spruce cover using soil charcoal

Anatomical identification of soil charcoal fragments was used to reconstruct the pre‐fire vegetation composition of a tree line site that burned ca 930 cal. AD in northern Québec, Canada. Soil charcoal was also used as a proxy to estimate black spruce Picea mariana palaeo‐cover. The site (a low‐elev...

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Bibliographic Details
Published in:Ecography
Main Authors: Asselin, Hugo, Payette, Serge
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2005
Subjects:
Online Access:http://dx.doi.org/10.1111/j.2005.0906-7590.04216.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.2005.0906-7590.04216.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.2005.0906-7590.04216.x
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Summary:Anatomical identification of soil charcoal fragments was used to reconstruct the pre‐fire vegetation composition of a tree line site that burned ca 930 cal. AD in northern Québec, Canada. Soil charcoal was also used as a proxy to estimate black spruce Picea mariana palaeo‐cover. The site (a low‐elevated hilltop) is presently devoid of spruce trees and dominated by dwarf birch Betula glandulosa , lichens, ericaceous shrubs ( Ledum decumbens , Vaccinium vitis‐idaea ) and sedges. In contrast, black spruce dominated before the fire with an understory of Empetrum nigrum and Vaccinium vitis‐idaea . Pre‐fire black spruce cover was estimated at 32%, giving an indication of the potential for warming‐induced natural reforestation of the forest‐tundra.