Boreal forest
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Transcript of Boreal forest
Boreal forest
Biophysical environmentsBiotic interactionsFire regimes & post-fire successionFloodplain succession & paludificationForest clearance and successionClimate change: natural &
anthropogenic
Boreal forest biome-------
Scandinavia70% Russia70% Alaska50% Canada
Fairbanks
Pr. AlbertKapuskasing
Chicoutimi
Note latitudinal variation
Boreal forest Tundra
Permafrostpatchy discontinuous continuous
Mean locationPolar FrontJulyJan
150 240 Mean #d <0°C
treegrowth
pollen/seedviability
120 30 Mean #d >10°C
non-accessed
spruce
pine
balsam fir
poplar
birch
other
Boreal forest vegetation types
(North America)
Boreal forest soils
south north
Podzols,
regosols
gleysols, cryosols
Underlain by coarse-textured deposits or bedrock. Well-drained, warm fairly rapidly in summer, more rapid breakdown of organics, strongly-leached, acidic, low nutrient availability.
Underlain by fine-textured deposits / permafrost. Poorly-drained, cold in summer; little microbial activity, slow breakdown of organics, low nutrient availability.
boreal forest taiga
% c
over
0
100
OAe
Bf
OBC
Cg
Forest community segregation in the boreal
forest
site: wet mesic drysoil: gleys podzolsactive: thin (<0.3m) thick (>2m)layer (or no permafrost)organic thick thin layer
blackspruce tamarack
white spruce -birch-aspen-
balsam fir
jack pine
mosses