This ecoregion is distinguished from the Central Canadian Shield Forests [NA0609] by a more maritime influence and balsam fir as the climatic climax species. The Eastern Canadian Forests characterize forested land in eastern Quebec, much of Newfoundland, and disjunct occurrences in the highlands of New Brunswick, and Cape Breton Island, Nova Scotia.
The ecoclimate of this ecoregion ranges from high and mid-boreal and perhumid mid-boreal to Oceanic, Atlantic, and maritime midboreal. Summers are generally cool, with average temperatures ranging between 8.5°C in the north to 14.5°C in the south. Winter temperatures vary according to proximity to the ocean and continental land mass. Thus, winters tend to be colder in Quebec and Labrador, particularly in the north, where mean temperatures range from -8°C to -13°C. On the Island of Newfoundland, winters are shorter and milder, where mean temperatures vary between -5.5°C to -1°C. Precipitation follows a similar pattern, there being less in the western, continental part of the ecoregion (800-1000 mm) than in the eastern and southern coastal areas and the Island of Newfoundland (1000-1200 mm in the north, 1200-1600 mm in the south). Coastal areas, especially in southeastern and northern Newfoundland and the Cape Breton Highlands, are particularly prone to heavy fog. Also, sea ice plays a significant role in the adjacent terrestrial climate of this ecoregion around the Strait of Belle Isle (ESWG 1995).
A wide range of physiographic features characterize this ecoregion, most of which are the result of glaciation. In the eastern part of the ecoregion, from Lac St. Jean south to the Gulf of St. Lawrence, and as far west as the Labrador coast, the region is underlain by massive Precambrian and Archean granites and gneisses, and lies between sea level and 600m asl. There are steep slopes that rise abruptly above the St. Lawrence river, and the interior of this part of the ecoregion is rolling or undulating and glacial drift-covered. Also, this portion of the ecoregion is incised by several large, wide river valleys. Isolated pockets of permafrost are found in some parts of this area, but become less common to the east and south. As one moves east toward the Atlantic coast, the surface becomes rougher, and surface deposits become thin and discontinuous, heavily influenced by fluvioglacial processes. The portions of the ecoregion in southeastern Labrador are also charcterized by deeply dissected margins. On the Island of Newfoundland, the physiography is also a result of glaciation, but rock outcrops also become common amidst hummocky, undulating, and sometimes ridged morainal deposits of varying thicknesses of sand or loam. The southern part of the island is part of the Appalachian peneplain, composed of a mix of soft, late, mostly unfolded Precacambrian sedimentary and volcanic rocks. On the Gaspé Peninsula and in the New Brunswick and Cape Breton Highlands, the Appalachian peneplain is also a factor, but is characterized by hummocky to mountainous terrain, underlain by folded Paleozoic sandstones and quartzites. Fluvioglacial deposits occur mostly in the valleys. This is some of the highest terrain on the east coast of Canada, and some peaks of the Appalachian range reach above 1000m asl in the Gaspe peninsula. Anticosti Island stands out in this ecoregion, as it is a south-dipping cuesta of Paleozoic carbonate strata, and relief rarely reaches 150m asl. Along the coastlines of the entire ecoregion differential erosion has played a significant role. Also, especially on the east coast of the Island of Newfoundland, the exposed bedrock terrain can slope up to a 30 percent grade (ESWG 1995).
The boreal forest in this bioregion is characterized by a mix of balsam fir (Abies balsamea) and black spruce (Picea mariana). Balsam fir dominates to the east as a result of the maritime influence of the Atlantic. Paper birch (Betula papyrifera), aspen (Populus tremuloides) and black spruce are typical of disturbed sites. White spruce (P. glauca) dominates in coastal areas where sea salt spray affects plant distributions. Moss-heath vegetation or barrens are also common in coastal areas affected by high winds. The warmer Lac St. Jean valley is dominated by mixedwoods more typical of southern climes (sugar maple (Acer saccharum), beech (Fagus grandifolia) and yellow birch (Betula alleghaniensis) on upland sites while eastern hemlock (Tsuga canadensis), balsam fir, eastern white pine (Pinus strobus), and white spruce prevail in valleys) (ESWG 1995).
The entire ecoregion provides prime habitat for many species, including moose (Alces alces), black bear (Ursus americanus), lynx (Lynx canadensis), and red fox (Vulpes vulpes). Woodland caribou (Rangifer tarandus ssp. caribou) can also be found through the area, with the exception of the New Brunswick and Cape Breton Highlands. In the central Laurentians, the northeastern portion of the ecoregion, snowshoe hare are common, and the wolf is an important predator. Marten (Martes americana), beaver (Castor canadensis), porcupine (Erethizon dorsatum), bobcat (Lynx rufus), and rabbit are common in the Appalachian regions. Goose, ptarmigan (Lagopus spp.) and ruffed grouse (Bonasa umbellus) are common in the north. Because of the length of coastline associated with this ecoregion, the area also supports a great variety of seabirds like murre (Uria spp.), eider (Somateria spp.), tern (Sterna spp.), and puffin (Fratercula spp.). In addition, seasonal bird populations vary significantly, as the eastern portion of the ecoregion is in the path of the Atlantic migratory flyway (ESWG 1995).
This ecoregion exhibits high levels of plant endemism in the Gulf of St. Lawrence with between 100 and 150 species. Maritime heath vegetation, a continentally unique plant assemblage, occurs in areas on the island of Newfoundland and the Gulf of St. Lawrence shore in Quebec. Large seabird colonies exist along the shorelines of this ecoregion.
Habitat Loss and Degradation
Approximately 40 percent of this ecoregion remains as intact habitat. The majority of this occurs along the northern portions of the ecoregion in Quebec. Parts of the ecoregion in the Gaspé, northern New Brunswick and Newfoundland have been heavily altered by a long history of human settlement. Some areas have been extensively logged and not returned to their original vegetation communities, often remaining as barrens or shrublands. Mining in some localized areas has also resulted in habitat loss (e.g. Matamec, Quebec).
Remaining Blocks of Intact Habitat
Most remaining habitat blocks are in the northern portions of the ecoregion. No major, intact habitat blocks remain in Newfoundland or the Gaspé outside of protected areas.
Degree of Fragmentation
Fragmentation of forest habitat is most notable. Little in the way of mature forest habitat remains throughout much of this ecoregion. Road networks through parts of the ecoregion (including logging roads) contribute to habitat fragmentation as well.
Degree of Protection
•Bay du Nord Provincial Wilderness Reserve - south-central Newfoundland - 2,895 km2
•Monts Valin Provincial Park - north of the Saguenay River, south-central Quebec
•Avalon Provincial Wilderness Reserve - eastern Newfoundland - 1,070 km2
•Cape Breton Highlands National Park - northern Nova Scotia - 950.53 km2
•Parc de la Gaspésie - eastern Quebec - 801.7 km2
•Middle Ridge Provincial Wildlife Reserve - south-central Newfoundland - 618 km2
•Terra Nova National Park - eastern Newfoundland - 405 km2
•Saguenay Provincial Park - south-central Quebec - 283.6 km2
•Polletts Cove, Aspy Fault Protected Area - Cape Breton Island, Nova Scotia - 275.66 km2
•Forillon National Park - eastern Quebec - 240.4 km2
Types and Severity of Threats
Logging is by far the most extensive threat to this ecoregion. In one logging license area in Quebec, 15,000 square kilometers of forest are scheduled to be logged in the coming 25 years. Logging elsewhere, combined with fuelwood harvest by coastal communities, has resulted in very little original forest remaining. Species composition has changed dramatically in historic times since European settlement of this region. Mining and mineral exploration are rapidly expanding in this ecoregion. Locally, peat extraction is of concern to some wetland habitats, particularly in Newfoundland.
Suite of Priority Activities to Enhance Biodiversity Conservation
•A Protected Areas Strategy has been launched in Newfoundland/Labrador. This needs to be implemented by the year 2000 with appropriate representative protected areas established. In the interim, the Little Grand Lake proposed ecological reserve needs to be designated.
?More protected areas are required for the Christmas Mountains and surrounding area in New Brunswick.
?Protected areas in Quebec that need to be established include:
?Rivière Vaureal watershed
?Harington Harbour shoreline habitat.
?Canadian Parks and Wilderness Society, Nova Scotia Chapter
?Cape Breton Naturalists Society
?Conservation Council of New Brunswick
?Federation of Nova Scotia Naturalists
?Friends of the Christmas Mountains National Park
?Heritage Foundation Terra Nova
?Les Amis de plein air de Cheticamp
?Margaree Environmental Society
?Natural History Society of Newfoundland and Labrador
?The Nature Conservancy, Quebec
?Nature Trust of New Brunswick
?New Brunswick Federation of Naturalists
?New Brunswick Protected Natural Areas Coalition
?Newfoundland/Labrador Environmental Association
?Nova Scotia Nature Trust
?Protected Areas Association of Newfoundland and Labrador
?Sierra Club, Cape Breton Group
?Tuckamore Wilderness Society
?UQCN - Union Québecoise pour la Conservation de la Nature
?World Wildlife Fund Canada, Quebec Region
Relationship to other classification schemes
This area corresponds to the terrestrial ecoregions of the Central Laurentians (TEC 101), the Mecatina Plateau (TEC 103), the northern Appalachians (TEC 117), and Anticosti Island (TEC 102). The Eastern Canadian Forests in Labrador cover the Paradise River and Lake Melville regions (TEC 104 and 105). On the Island of Newfoundland, ecoregions include the Strait of Belle Isle (TEC 106), the Northern Peninsula (TEC 107), the Maritime Barrens (TEC 114), the Avalon Forest (TEC 115) and Southwestern, Central, and Northeastern Newfoundland (TEC 109, 112 and 113). In New Brunswick, the New Brunswick Highlands (TEC 119) are home to Eastern Canadian Forests, and in Nova Scotia, the Cape Breton Highlands (TEC 129) are as well (Ecological Stratification Working Group 1995).
The Eastern Canadian Forests area is also characterized by numerous Rowe (1972) forest regions and sections. Boreal forest sections include: Laurentide-Onatchiway, Chibougamau-Natashquan, Gaspé, Hamilton and Eagle Valleys, Northeastern Transition, Grand Falls, Corner Brook, Anticosti, Northern Peninsula, Avalon, Newfoundland-Labrador Barrens and Forest-Tundra 1a and b, 2, 12, 13a, 28a, 28b, 28c, 29-32). In this part of the Acadian forest region are the New Brunswick Uplands and the Cape Breton Plateau (1 and 6). The Saguenay section (7) of the Great Lakes-St. Lawrence forests is also part of the Eastern Canadian Forests.
Prepared by: B. Meades, L. Gratton, A. Perera, N. Zinger, L. Jackson, J. Goltz, C. Stewart, K. Kavanagh, M. Sims, G. Mann.