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CEGL000273 Abies grandis / Coptis occidentalis Forest
Type Concept Sentence: No Data Available
Common (Translated Scientific) Name: Grand Fir / Idaho Goldthread Forest
Colloquial Name: No Data Available
Hierarchy Level: Association
Type Concept: This plant association is known from stands located between the South Fork of the Clearwater and Salmon rivers, within the Idaho Batholith ecoregional section. The mountainous region possesses a Pacific maritime-influenced climatic regime. Winters are mild and moist; summers are dry. The association occurs on steep, north-facing slopes in upper-slope positions at 1585 to 1650 m (5200-5400 feet) elevation. Soils are generally shallow, but may have a significant component of volcanic ash, especially in the upper layers. Pinus contorta, Pinus ponderosa, or Larix occidentalis often dominate early- and mid-seral stands. Pseudotsuga menziesii is often dominant in the forest overstory in late-seral stands. A low-shrub layer is well-developed and dominated by Vaccinium membranaceum, with minor amounts of Rubus parviflorus, Lonicera utahensis and Chimaphila umbellata. The herbaceous layer is dominated by perennial forbs, with Coptis occidentalis being the most abundant. Several other species are indicative of the cool, moist conditions beneath the overstory: Galium triflorum, Viola orbiculata, Mitella stauropetala and Thalictrum occidentale.
Diagnostic Characteristics: No Data Available
Rationale for Nominal Species or Physiognomic Features: No Data Available
Classification Comments: Steele et al. (1976) identified this type habitat type in central Idaho on the Nez Perce National Forest. Cooper et al. (1987) also recognized the type in central Idaho but split it into two phases: a colder, higher elevation Coptis occidentalis phase and a warmer, lower elevation Physocarpus malvaceus phase.
Similar NVC Types: No Data Available
note: No Data Available
Physiognomy and Structure: No Data Available
Floristics: This is a forest association, dominated by evergreen needle-leaved trees. Pseudotsuga menziesii or Picea engelmannii dominate most mature stands, with Abies grandis and Picea successfully reproducing in the understory layer as seedlings, saplings and small trees. Early-successional stages may be dominated by Pinus ponderosa, Pinus contorta, or the deciduous needle-leaved Larix occidentalis. Abies grandis and Picea are always present. A low-shrub layer is well-developed and dominated by deciduous broad-leaved species, primarily Vaccinium membranaceum (= Vaccinium globulare), with minor amounts of Rubus parviflorus, Lonicera utahensis, and Chimaphila umbellata. The herbaceous layer is dominated by perennial forbs, with Coptis occidentalis being the most abundant. Several other species are indicative of the cool, moist conditions beneath the overstory, such as Galium triflorum, Viola orbiculata, Mitella stauropetala, and Thalictrum occidentale. Slightly moister sites within the type may be defined by Clintonia uniflora, Maianthemum stellatum, and Tiarella trifoliata var. unifoliata (Johnson and Simon 1987).
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. Indian paint fungus (Echinodontium tinctorium) may be very common on grand fir within this type (Pfister et al. 1977). Larix occidentalis can be subject to attack by the dwarf mistletoe parasite.
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.
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 alliance is found in a mountainous region with a climate moderated by maritime influence, particularly in the winter and spring. Precipitation typically occurs as prolonged gentle rains, with periods of fog and heavy cloud cover. During summer, the maritime influence is weak; these months are dry and have daily extremes of temperature. This association is described as occupying steep, north-facing drainage headland sideslopes, from 1585 to 1645 m (5200-5400 feet) elevation. Soils are generally shallow, but may have a significant component of volcanic ash, especially in the upper layers. Seeps may occur in some stands.
This is a moist, cool type. Although no climatic data are available, the location of this type in Idaho and Oregon subjects it to a maritime climate during winter and early spring which moderates its temperature and environment for plant growth through prolonged, gentle rainfall interspersed with periods of fog and heavy cloud cover. In late spring, the maritime influence diminishes and is replaced by a continental climate characterized by warm days and cold nights. Small amounts of precipitation are delivered in brief downpours. This results in plant species tolerating greater summer drought and severely fluctuating temperatures.
This is a moist, cool type. Although no climatic data are available, the location of this type in Idaho and Oregon subjects it to a maritime climate during winter and early spring which moderates its temperature and environment for plant growth through prolonged, gentle rainfall interspersed with periods of fog and heavy cloud cover. In late spring, the maritime influence diminishes and is replaced by a continental climate characterized by warm days and cold nights. Small amounts of precipitation are delivered in brief downpours. This results in plant species tolerating greater summer drought and severely fluctuating temperatures.
Geographic Range: This association is located in central Idaho and northeastern Oregon. A few isolated sites of this plant association are located between the South Fork of the Clearwater and the Salmon rivers, within the Idaho Batholith ecoregional section, and in northeastern Oregon in the Wallowa-Snake Province of the Wallowa-Whitman National Forest.
Nations: US
States/Provinces: ID, OR
Plot Analysis Summary:
http://vegbank.org/natureserve/ELEMENT_GLOBAL.2.683583
Confidence Level: Moderate
Confidence Level Comments: No Data Available
Grank: G2
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 | CEGL000273 Grand Fir / Idaho Goldthread Forest | CEGL000273 | 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 / Coptis occidentalis Habitat Type (Cooper et al. 1987)
? Abies grandis / Coptis occidentalis Habitat Type (Johnson and Simon 1987) [found in the Wallowa-Snake Province of northeastern Oregon from 5200-5400 feet.]
? Abies grandis / Coptis occidentalis Habitat Type (Steele et al. 1981) [found in central Idaho on the Payette, Salmon, and Nez Perce national forests.]
? Abies grandis / Xerophyllum tenax Habitat Type, Coptis occidentalis Phase (Cooper et al. 1987)
? Abies grandis / Coptis occidentalis (Johnson and Simon 1985) [found in the Hells Canyon National Recreation Area of northeast Oregon between 5200-5400 feet.]
? Abies grandis / Coptis occidentalis Habitat Type (Johnson and Simon 1987) [found in the Wallowa-Snake Province of northeastern Oregon from 5200-5400 feet.]
? Abies grandis / Coptis occidentalis Habitat Type (Steele et al. 1981) [found in central Idaho on the Payette, Salmon, and Nez Perce national forests.]
? Abies grandis / Xerophyllum tenax Habitat Type, Coptis occidentalis Phase (Cooper et al. 1987)
? Abies grandis / Coptis occidentalis (Johnson and Simon 1985) [found in the Hells Canyon National Recreation Area of northeast Oregon between 5200-5400 feet.]
- 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]
- 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., Jr., and S. A. Simon. 1987. Plant associations of the Wallowa-Snake Province Wallowa-Whitman National Forest. Technical Paper R6-ECOL-TP-255A-86. USDA Forest Service, Pacific Northwest Region, Wallowa-Whitman National Forest. 399 pp. plus appendices.
- Johnson, C. G., and S. A. Simon. 1985. Plant associations of the Wallowa Valley Ranger District, Part II: Steppe. USDA Forest Service, Pacific Northwest Region, Wallowa-Whitman National Forest. 258 pp.
- 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.
- Pfister, R. D., B. L. Kovalchik, S. F. Arno, and R. C. Presby. 1977. Forest habitat types of Montana. General Technical Report INT-34. USDA Forest Service, Intermountain Forest and Range Experiment Station, Ogden, UT. 174 pp.
- Steele, R., R. D. Pfister, R. A. Ryker, and J. A. Kittams. 1981. Forest habitat types of central Idaho. General Technical Report INT-114. USDA Forest Service, Intermountain Forest and Range Experiment Station, Ogden, UT. 138 pp.
- 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.