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Growth of black spruce and tamarack in peatlands is generally dependent on variations in the water table. In fact, in spruce-sphagnum-ericaceous forests, variations in water table constitute a major obstacle to root development and the normal functioning of the tree. This report presents a dendrochronological analysis of relations between climate and volume increment of black spruce and tamarack in drained peatlands at Saint-Anaclet, near Rimouski.
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