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CEGL000269 Abies grandis / Asarum caudatum Forest
Type Concept Sentence: No Data Available
Common (Translated Scientific) Name: Grand Fir / British Columbia Wild Ginger Forest
Colloquial Name: No Data Available
Hierarchy Level: Association
Type Concept: This evergreen forest association is found on all terrain, usually on protected exposures or cove-like situations, on the drainages of the Clearwater River in northern Idaho between 671 and 1814 m (2200-5950 feet) elevation. Parent materials vary, but granitics and metasediments are the most common. Volcanic ash influences the upper horizons of most of the profiles. Soil textures are primarily silt loams and silty clay loams with only traces of exposed soil or rock. Gravel content is usually less than 30%. The effective rooting depth averages 50 cm with an average pH of 6.3. Abies grandis is the indicated climax tree species. Pseudotsuga menziesii along with Picea engelmannii (at the higher elevations) are the major seral tree species. Following disturbance, sites are frequently recolonized by Abies grandis, leading to even-aged stands dominated by a climax species. Occasional species are Pinus monticola, Pinus ponderosa, and Larix occidentalis. The shrub-layer species typically demonstrate low cover values. Species with high constancy are Acer glabrum, Rosa gymnocarpa, and Symphoricarpos albus. Their coverage declines with increasing stand age and canopy cover. There is high species richness and undergrowth coverage in the forb layer due to the moderate environment of this type. Asarum caudatum is diagnostic for this type. Clintonia uniflora, Tiarella trifoliata, and Maianthemum stellatum are characteristically present. Other forbs, such as Coptis occidentalis, Prosartes hookeri, Polystichum munitum, or Synthyris platycarpa, may occasionally dominate this layer.
Diagnostic Characteristics: No Data Available
Rationale for Nominal Species or Physiognomic Features: No Data Available
Classification Comments: Some of Daubenmire''s (1968) Abies grandis / Paxistima myrsinites and at least one stand of Williams and Lillybridge''s (1985) Abies grandis / Clintonia uniflora are similar to this association. Steele et al. (1976) first described this type for the Nez Perce National Forest.
Similar NVC Types: No Data Available
note: No Data Available
Physiognomy and Structure: No Data Available
Floristics: Abies grandis is the indicated climax tree species. Pseudotsuga menziesii along with Picea engelmannii (at the higher elevations) are the major seral tree species. Following disturbance, sites are frequently recolonized by Abies grandis, leading to even-aged stands dominated by a climax species. Occasional species are Pinus monticola, Pinus ponderosa, and Larix occidentalis. The shrub-layer species typically demonstrate low cover values. Species with high constancy are Acer glabrum, Rosa gymnocarpa, and Symphoricarpos albus. Their coverage declines with increasing stand age and canopy cover. There is high species richness and undergrowth coverage in the forb layer due to the moderate environment of this type. Asarum caudatum is diagnostic for this type. Clintonia uniflora, Tiarella trifoliata, and Maianthemum stellatum (= Smilacina stellata) are characteristically present. Other forbs, such as Coptis occidentalis, Prosartes hookeri (= Disporum hookeri), Polystichum munitum, or Synthyris platycarpa, may occasionally dominate this layer.
Cooper et al. (1991) recognize three phases of this type. The first, the Asarum caudatum typic phase, ranges from 640-1645 m (2100-5400 feet). It occupies gentle to steep slopes of all aspects, with warmer exposures more frequently represented. Coverage of forbs and warm-site shrubs such as Symphoricarpos albus, Holodiscus discolor, and Physocarpus malvaceus is increased relative to that found on the other phases, and persists late into the sere. Abies grandis and Pseudotsuga generally codominate seral stages. Cooper''s second phase is a Menziesia ferruginea phase occurring on the coolest upper elevations (greater than 1340 m [4400 feet]) with sites usually confined to steep northwest- through east-facing slopes or benchlands. A layer of Menziesia ferruginea dominates a tall-shrub stratum, which may include abundant Taxus brevifolia and Vaccinium membranaceum (= Vaccinium globulare). These sites have the greatest potential for supporting several seral tree species such as Picea engelmannii and Pseudotsuga. Cooper''s third phase is a Taxus brevifolia phase. This phase has been found only on the Nez Perce National Forest from 1220-1705 m (4000-5600 feet). It is most prevalent on moderate to steep slopes with warm, often protected exposures and ridgetop benches. Taxus brevifolia dominates the tall-shrub/small-tree layer, becoming so dense that some herbs, tree seedlings, and smaller shrubs are eliminated.
Cooper et al. (1991) recognize three phases of this type. The first, the Asarum caudatum typic phase, ranges from 640-1645 m (2100-5400 feet). It occupies gentle to steep slopes of all aspects, with warmer exposures more frequently represented. Coverage of forbs and warm-site shrubs such as Symphoricarpos albus, Holodiscus discolor, and Physocarpus malvaceus is increased relative to that found on the other phases, and persists late into the sere. Abies grandis and Pseudotsuga generally codominate seral stages. Cooper''s second phase is a Menziesia ferruginea phase occurring on the coolest upper elevations (greater than 1340 m [4400 feet]) with sites usually confined to steep northwest- through east-facing slopes or benchlands. A layer of Menziesia ferruginea dominates a tall-shrub stratum, which may include abundant Taxus brevifolia and Vaccinium membranaceum (= Vaccinium globulare). These sites have the greatest potential for supporting several seral tree species such as Picea engelmannii and Pseudotsuga. Cooper''s third phase is a Taxus brevifolia phase. This phase has been found only on the Nez Perce National Forest from 1220-1705 m (4000-5600 feet). It is most prevalent on moderate to steep slopes with warm, often protected exposures and ridgetop benches. Taxus brevifolia dominates the tall-shrub/small-tree layer, becoming so dense that some herbs, tree seedlings, and smaller shrubs are eliminated.
Dynamics: Damping-off fungus takes a heavy toll of Abies grandis seedlings during wet seasons, and insolation and drought cause mortality during the dry summer months. Seedlings are well-established by the third year. Fire hazard is normally low to moderate under normal weather conditions (Fischer and Bradley 1987). Although this type does not occur in Fischer and Bradley''s study, this type is equivalent to their Group Eleven - warm, moist grand fir, western red-cedar, and western hemlock habitat types. The threat of fire is highest in the summer, when the moist maritime climate no longer prevails. During severe summer drought, heavy fuel loading from high plant productivity can set the stage for severe, widespread fires. Stands are replaced and sites revert to pioneer species. Summertime fuel-moisture conditions in young stands are not nearly as high as in older more dense stands, and the effects of fire are often more severe than they are in older stands. Surface fires often scar the base of the grand fir, creating favorable entry points for decay organisms. The initial floral component, seeds stored on site, and the accidents of natural seeding and seedling establishment, may structure the community following the fire more than the characteristics of the fire itself. Although generally true for all fire groups, it is more pronounced in this fire group. The use of fire for site preparation will usually result in increased spring and summer browse for big game in addition to successful regeneration of seral tree species.
Environmental Description: This association is found on all terrain, usually on protected exposures or cove-like situations, on the drainages of the Clearwater River between 671 and 1814 m (2200-5950 feet) elevation. Parent materials vary, but granitics and metasediments are the most common. Volcanic ash influences the upper horizons of most of the profiles. Soil textures are primarily silt loams and silty clay loams with only traces of exposed soil or rock. Gravel content is usually less than 30%. The effective rooting depth averages 50 cm with an average pH of 6.3.
This is a warm moist type. Although no precise climatic data are available, the climate in which this type occurs is dominated by the inland maritime regime. This regime brings prolonged gentle rains and deep snow accumulations at higher elevations during winter and spring, with abundant cloudiness, fog, and high humidity. This makes for mild, moderate winters. Summers are very dry, usually less than one inch of precipitation per month.
This is a warm moist type. Although no precise climatic data are available, the climate in which this type occurs is dominated by the inland maritime regime. This regime brings prolonged gentle rains and deep snow accumulations at higher elevations during winter and spring, with abundant cloudiness, fog, and high humidity. This makes for mild, moderate winters. Summers are very dry, usually less than one inch of precipitation per month.
Geographic Range: This association is found in northern Idaho.
Nations: US
States/Provinces: ID, MT, OR
Plot Analysis Summary:
http://vegbank.org/natureserve/ELEMENT_GLOBAL.2.687552
Confidence Level: Low - Poorly Documented
Confidence Level Comments: No Data Available
Grank: G4
Greasons: No Data Available
Type | Name | Database Code | Classification Code |
---|---|---|---|
Class | 1 Forest & Woodland Class | C01 | 1 |
Subclass | 1.B Temperate & Boreal Forest & Woodland Subclass | S15 | 1.B |
Formation | 1.B.2 Cool Temperate Forest & Woodland Formation | F008 | 1.B.2 |
Division | 1.B.2.Nb Rocky Mountain Forest & Woodland Division | D194 | 1.B.2.Nb |
Macrogroup | 1.B.2.Nb.3 Western Hemlock - Grand Fir - Western Larch Mesic Lower Montane Forest Macrogroup | M500 | 1.B.2.Nb.3 |
Group | 1.B.2.Nb.3.a Grand Fir - Douglas-fir - Western Larch Central Rocky Mountain Forest Group | G211 | 1.B.2.Nb.3.a |
Alliance | A3362 Grand Fir - Douglas-fir Central Rocky Mountain Forest & Woodland Alliance | A3362 | 1.B.2.Nb.3.a |
Association | CEGL000269 Grand Fir / British Columbia Wild Ginger Forest | CEGL000269 | 1.B.2.Nb.3.a |
Concept Lineage: No Data Available
Predecessors: No Data Available
Obsolete Names: No Data Available
Obsolete Parents: No Data Available
Synonomy: = Abies grandis / Asarum caudatum Habitat Type (Cooper et al. 1987) [found in northern Idaho on the drainages of the Clearwater River between 671-1814 m (2200-5950 feet) elevation.]
? Abies grandis / Clintonia uniflora (Williams and Lillybridge 1985)
? Abies grandis / Paxistima myrsinites (Daubenmire 1968a)
? Abies grandis / Clintonia uniflora (Williams and Lillybridge 1985)
? Abies grandis / Paxistima myrsinites (Daubenmire 1968a)
- Bourgeron, P. S., and L. D. Engelking, editors. 1994. A preliminary vegetation classification of the western United States. Unpublished report. The Nature Conservancy, Western Heritage Task Force, Boulder, CO. 175 pp. plus appendix.
- Cooper, S. V., K. E. Neiman, R. Steele, and D. W. Roberts. 1987. Forest habitat types of northern Idaho: A second approximation. General Technical Report INT-236.USDA Forest Service, Intermountain Research Station, Ogden, UT. 135 pp. [reprinted in 1991]
- Daubenmire, R. 1968a. Analysis and description of plant communities. Pages 62-70 in: Plant communities: A text book of plant synecology. Harper & Row, New York.
- Fischer, W. C., and A. F. Bradley. 1987. Fire ecology of western Montana forest habitat types. General Technical Report INT-223. USDA Forest Service, Intermountain Research Station, Ogden, UT. 95 pp.
- Johnson, C. G., and R. R. Clausnitzer. 1992. Plant associations of the Blue and Ochoco mountains. R6-ERW-TP-036-92. USDA Forest Service, Pacific Northwest Region, Wallowa-Whitman National Forest. 163 pp. plus appendices.
- Kagan, J. S., J. A. Christy, M. P. Murray, and J. A. Titus. 2004. Classification of native vegetation of Oregon. January 2004. Oregon Natural Heritage Information Center, Portland. 52 pp.
- MTNHP [Montana Natural Heritage Program]. 2002b. List of ecological communities for Montana. Montana Natural Heritage Program, Montana State Library, Helena, MT.
- Steele, R., S. F. Arno, and R. D. Pfister. 1976. Preliminary forest habitat types of the Nezperce National Forest. Unpublished report by USDA Forest Service, Intermountain Forest and Range Experiment Station, Ogden, UT. 71 pp.
- Western Ecology Working Group of NatureServe. No date. International Ecological Classification Standard: International Vegetation Classification. Terrestrial Vegetation. NatureServe, Boulder, CO.
- Williams, C. K., and T. R. Lillybridge. 1985. Forested plant associations of the Colville National Forest. Draft. Unpublished field guide prepared for USDA Forest Service.