Eastern forest-boreal transition
The Eastern forest-boreal transition is a temperate broadleaf and mixed forests ecoregion of North America, mostly in eastern Canada. It is a transitional zone or region between the predominantly coniferous Boreal Forest and the mostly deciduous broadleaf forest region further south.
|Eastern forest-boreal transition|
|Biome||Temperate broadleaf and mixed forests|
|Borders||Eastern Canadian forests, Eastern Great Lakes lowland forests, Central Canadian Shield forests and Western Great Lakes forests|
|Countries||United States and Canada|
|States/Provinces||New York, Ontario and Quebec|
- 1 Location and climate
- 2 Flora
- 3 Fauna
- 4 Threats and preservation
- 5 See also
- 6 References and external links
Location and climateEdit
The ecoregion includes most of the southern Canadian Shield in Ontario and Quebec north and west of the Saint Lawrence River lowlands. The portion in Northeastern Ontario includes the eastern shores of Lake Superior, Greater Sudbury, North Bay, Ontario, Lake Nipissing, the Clay Belt and Temagami. Areas in Central Ontario include Muskoka, Parry Sound, Algonquin Park, and Haliburton. The Quebec portion takes in Lake Timiskaming, the southern Laurentian Mountains, Quebec City, the Saguenay River, and Saguenay, Quebec. There is a separate section of the ecoregion in the Adirondack Mountains in upper New York State, United States. However the higher elevations of the Laurentian Mountains and the northern Appalachian Mountains in Canada constitute the Eastern Canadian forests ecoregion.
The flora in this ecoregion varies considerably based on soil conditions and elevation. These mixed forests are distinct from the deciduous forests south of the Canadian Shield and the cooler boreal forests to the north.
Conifer swamps occur in areas that are seasonally flooded. Trees can be very dense or sparse; mats of sphagnum moss cover the ground. Black spruce (Picea mariana) and tamarack (Larix laricina) are the predominant tree species. Where the soil is not saturated year round grows northern white cedar (Thuja occidentalis). Speckled alder (Alnus incana) grows around the edges of these swamps and red spruce (Picea rubens) and white pine (Pinus strobus) grow on higher, drier ground.
Lowland conifer forestsEdit
Lowland conifer forests occur on flats, low ridges, and knolls near bodies of water. They are dominated by balsam fir (Abies balsamea) and red spruce, although white pine and paper birch (Betula papyrifera) also occur. The ground is often stony with little vegetation.
Hardwood-conifer mixed forestsEdit
Hardwood-conifer mixed forests occur in a transition zone between lowland conifer and northern hardwood forests. The ground is less rocky than in the lowland conifer forests and thus supports more vegetation. Trees include red spruce, balsam fir, eastern hemlock (Tsuga canadensis), red maple (Acer rubrum), and yellow birch (Betula alleghaniensis). The understory vegetation is abundant, with witchhobble (Viburnum lantanoides), honeysuckle (Lonicera spp.), and striped maple (Acer pensylvanicum). The herbaceous layer include common wood sorrel (Oxalis spp.), bunchberry (Cornus canadensis), yellow clintonia (Clintonia borealis), ferns, and mosses.
Northern hardwood forestsEdit
Northern hardwood forests occur on the richest, most productive soils. Sugar maple (Acer saccharum), American beech (Fagus grandifolia), and yellow birch are the predominant tree species. In secondary forests, red spruce, white pine, white ash (Fraxinus americana), eastern hemlock, black cherry (Prunus serotina), and red maple are present. Witchhobble (Viburnum alnifolium) is a common understory shrub. Ferns and clubmosses grow in the herbaceous layer, along with numerous species of spring-flowering forbs.
Upper slope hardwood-conifer mixed forestsEdit
Upper slope hardwood-conifer mixed forests are an area of transition between the northern hardwood and the mountain conifer forests. They are similar to hardwood-conifer forests, but with no red maple. Red spruce and eastern hemlock, together with sugar maple, yellow birch, and American beech are the dominant species, with scattered white pine.
Mountain conifer forestsEdit
Red spruce and balsam fir are common at lower elevations of the mountain conifer forests. Hardwoods that grow among the conifers include paper birch, yellow birch, and American mountain-ash (Sorbus americana). With increasing elevation, balsam fir becomes more abundant. Near treeline, black spruce joins balsam fir in the krummholz. Herbaceous plants include wood sorrel, bunchberry, yellow clintonia, and spinulose woodfern (Dryopteris carthusiana). Mosses and lichens cover exposed rocks.
Rocks are exposed and covered with lichens and mosses. Low-lying plants more common in the tundra to the north grow here. They include gold-colored deer’s hair (Trichophorum cespitosum), alpine bilberry (Vaccinium uliginosum), lapland rosebay (Rhododendron lapponicum), bearberry willow (Salix uva-ursi), mountain sandwort (Minuartia groenlandica), and alpine holygrass (Hierochloe alpina). In the Adirondacks, these communities are limited to 85 acres (34 ha) on 11 peaks.
Old-growth forest such as the pinewoods found in this ecoregion are home to a complex variety of long-established wildlife including many invertebrates and reptiles and birds such as American black duck (Anas rubripes), wood duck (Aix sponsa), hooded merganser (Lophodytes cucullatus), and pileated woodpecker (Dryocopus pileatus).
Mammals found here include the North American cougar (Puma concolor), moose (Alces alces), American black bear, Canada lynx (Lynx canadensis), snowshoe hare (Lepus americanus), wolf (Canis lupus), coyote (Canis latrans) and white-tailed deer (Odocoileus virginianus).
The Lake Nipissing area in particular is home to eastern chipmunk (Tamias striatus), mourning dove (Zenaida macroura), northern cardinal (Cardinalis cardinalis), and wood thrush (Hylocichla mustelina).
Threats and preservationEdit
These forests have been severely damaged by centuries of clearance for timber, roads, agricultural and urban development. This development now includes ski facilities, while logging and mining are ongoing. Protected areas include: Papineau-Labelle Wildlife Reserve, Mont-Tremblant, Jacques-Cartier, Hautes-Gorges-de-la-Rivière-Malbaie and La Mauricie National Parks in Quebec; Algonquin Provincial Park, Lake Superior Provincial Park, Lady Evelyn-Smoothwater Provincial Park, French River Provincial Park, Killarney Provincial Park and a number of parks in Algoma District in Ontario; and Adirondack Park in New York. Adirondack Park contains the largest areas of original red pine and eastern white pine in the world and one of the largest areas of original forest in the United States, the Five Ponds Wilderness Area.
- Hoekstra, J. M.; Molnar, J. L.; Jennings, M.; Revenga, C.; Spalding, M. D.; Boucher, T. M.; Robertson, J. C.; Heibel, T. J.; Ellison, K. (2010). Molnar, J. L. (ed.). The Atlas of Global Conservation: Changes, Challenges, and Opportunities to Make a Difference. University of California Press. ISBN 978-0-520-26256-0.
- "Eastern forest-boreal transition". Terrestrial Ecoregions. World Wildlife Fund.
- "Adirondack Forest Communities". State University of New York College of Environmental Science and Forestry. 2010.
- "Eastern Forest-Boreal Transition". Terrestrial Ecoregions. World Wildlife Fund.
- World Wildlife Fund, ed. (2001). "Eastern Forest-Boreal Transition". WildWorld Ecoregion Profile. National Geographic Society. Archived from the original on 2010-03-08.
- Central U.S. hardwood forests images at bioimages.vanderbilt.edu