top of page

Post-Glacial Vegetation (the present!)

It is theorized that approximately 5,000 years ago, the Canadian boreal forest resembled current forest stand structures for the most part. It never truly stayed at an equilibrium, but the distribution would have shifted up and down from it's current position. The general structure of the boreal taiga in North American regions today consists of forest-tundra (Pink on map below) at the most Northern limit. Further south the structure transitions into open lichen woodland (Red on map below), eventually leading into closed canopy (Light green on map below) further South.

Most trees native to the Canadian boreal taiga are conifers. These species include Black, Spruce, Balsam Fir in more eastern regions, White Spruce, Tamarack, and Lodgepole and Jack pine. Some deciduous species include certain Aspen, Birch, and Poplar.

Many areas of the Canadian Boreal forest consist of large stands of Black Spruce. These conifers are tolerant of permafrost, shallow soils, and areas with high soil saturation (waterlogged). Much shrub understory of the Boreal forest belongs to the Ericaceae family.  These species of shrubs can tolerate soils which are flooded, acidic, or nutrient poor. Examples of these shrubs would be Sheep Laurel and Labrador Tea.​

White Spruce.

Taken from Macphail Woods Ecological Forestry Project ©

Balsam Poplar.

Taken from the Tree Conpendium ©

Different Forest Composition.

Taken from the Canadian Atlas Online ©

BOREAL @ MEMORIAL

bottom of page