Trembling aspen (Populus tremuloides) in western Canadian boreal forests is
generally believed to occur as young, even-aged stands, as part of a fire-
dominated landscape. However, the available quantitative estimates of the r
ate of disturbance by fire in this region differ markedly. One estimate is
consistent with forests much older than are currently thought to exist. The
theory of gap dynamics may partly reconcile the discrepancy, by suggesting
a mechanism whereby old, uneven-aged aspen stands could develop and persis
t.
We surveyed for canopy gaps in 43-67 yr old aspen stands in northeastern Al
berta, Canada, and found that expanded gaps occupy 3.6-16.6% of stand area,
increasing linearly with stand age over the sampled range. Gaps begin to f
orm similar to 40 yr after stand initiation, through the accumulated mortal
ity of adjacent canopy trees. The densities of aspen (P. tremuloides), bals
am poplar (P. balsamifera), and paper birch (Betula papyrifera a) saplings
were 2-3 times higher in gaps than in paired control areas under a closed c
anopy. Sample plots in order aspen stands in the vicinity had spatially het
erogeneous, uneven age structures, consistent with gap dynamics. More exten
sive samples of stem-size-structure data and forest-inventory data sets ind
icate that this phenomenon is widespread. We conclude that gap dynamics can
maintain near-pure deciduous stands in this region, in the absence of shad
e-tolerant competitors. a cellular-automata model of aspen-stand dynamics,
with spatially random mortality, yields predictions consistent with our eth
er results. It follows from the model that stable age structures develop wi
thin 250-300 yr, that mean canopy age is a biased estimator of stand age in
stands older than 100 yr, and that small-sample maxims have unfavorable sa
mpling distributions. Comparable biases may be present in ages estimated fr
om aerial photography: significant areas of "young" aspen have age structur
es characteristic of simulated old stands. We present less direct arguments
that other components of the Alberta boreal forest are also older than is
generally thought, and we outline a new model of the regional forest dynami
cs. We conclude that vast tracts of boreal forest are now being managed on
the basis of an incorrectly estimated age structure and a misconception of
their landscape dynamics.