L. Archambault et al., FOREST SUCCESSION FOLLOWING A FIRE IN A B ALSAM FIR YELLOW BIRCH STAND IN THE BAS-SAINT-LAURENT REGION OF QUEBEC, Forestry Chronicle, 73(6), 1997, pp. 702-710
Forest successions following a forest fire that occurred in 1932 were
studied on mesic sites of the boreal mixedwood forest of the Bas-Saint
-Laurent region of Quebec, Canada. Physiographic, soil and vegetation
data were collected in 28 ecosystems distributed on a topographic grad
ient. The vegetation composition of the main canopy, 64 years after th
e fire, varied according to topographic situation, The proportion of t
olerant hardwood species (yellow birch (Betula alleghaniensis Britton)
, sugar maple (Acer saccharum, Marsh.), red maple (Acer rubrum, L.)) i
ncreased toward upper slopes whereas it was the opposite fur coniferou
s species (white spruce (Picea glauca [Moench] Voss), balsam fir (Abie
s balsamea [L.] Mill.)), as their proportion increased toward lower sl
opes. Intolerant hardwood species (white birch (Betula!la papyrifera M
arsh.), trembling aspen (Populus tl el,tremuloides Michx.)) were abund
ant in all ecosystems. The distribution pattern of regeneration densit
y and stocking of tolerant hardwoods and conifers was similar to that
of the main canopy. The majority of commercial species, including tole
rant species, established rapidly after the fire. Only eastern white c
edar (Thuya?! occidentalis L.), which is a species typical of late suc
cession, did not grow back. Ten years after the fin, 78% of the sample
d dominant trees were established. Competition caused by mountain mapl
e (Acer spicatum Lam.) did not seem to be as important after fire comp
ared with the situation after clearcutting. Results showed that after
the elimination of intolerant species, the vegetation composition shou
ld evolve toward the potential vegetation (climax) of the toposequence
, that is, the sugar maple - yellow birch type on upper slopes, the ba
lsam fir - yellow birch type on midslopes and the balsam fir - yellow
birch - cedar type on lower slopes.