Print Report
CEGL005895 Abies lasiocarpa - Picea engelmannii / Menziesia ferruginea / Xerophyllum tenax Forest
Type Concept Sentence: No Data Available
Common (Translated Scientific) Name: Subalpine Fir - Engelmann Spruce / Rusty Menziesia / Common Beargrass Forest
Colloquial Name: No Data Available
Hierarchy Level: Association
Type Concept: This association occurs throughout the middle to northern Rocky Mountains and on into the Canadian Rockies as a small- to large-patch type from mid to upper subalpine habitats. In the southerly portions of its distribution, the Wallowa and Seven Devils mountains and Idaho Batholith, it faithfully occupies moderate to steep slopes of northerly aspects at elevations ranging from 1700 to 2300 m (5600-7500 feet), but dropping to 1370 m (4500 feet) where frost pocket conditions obtain. Further to the north it also occurs predominantly on northerly exposures, but at higher elevations in wetter climates, it may be found on southerly exposures. It can occur on a given slope from the toe, up the backslope to the slope shoulder, and in wetter climates is found on ridgetops as well. It is perhaps most widely distributed in western Montana where individual stands may comprise hundreds to thousands of acres. It exhibits no particular substrate preferences being found on granitics, fine-grained sedimentaries (including argillite and limestone), metasediments, and mica-schist; volcanic ash caps of varying depths (to 50 cm thickness) are very prevalent in the southern and western portions. The predominant soil texture is silt loam, and soils are uniformly well-drained. Rock content of surface horizons ranges from about 15% to over 50%. This is a closed forest type for the most part with total upper canopy cover ranging upward from 60%. A variable mix of Abies lasiocarpa and Picea engelmannii dominates the canopy as well as the regeneration layers. Seral tree species do poorly on these sites; Pinus contorta, Pseudotsuga menziesii, and Larix occidentalis are the only tree species consistently present and seldom is their canopy cover as great as 20%. The modal condition for the undergrowth varies with geographic region. Menziesia ferruginea consistently dominates the tall-shrub layer, which may also have Alnus viridis ssp. sinuata as a conspicuous component. In all parts of the type''s range Vaccinium membranaceum is the mid (short) shrub dominant with coverages generally upwards of 30%; it is usually accompanied by low cover of Ribes lacustre and the somewhat shorter dwarf-shrub Vaccinium scoparium (or its ecological analogue Vaccinium myrtillus). The only graminoid consistently present, Luzula glabrata, occurs in slightly greater than trace amounts in stands at higher elevations and experiencing deeper snowpack. The herb layer, depauperate in comparison to that of ~Abies lasiocarpa - Picea engelmannii / Menziesia ferruginea / Clintonia uniflora Forest (CEGL005893)$$, is strongly dominated by Xerophyllum tenax; Arnica cordifolia, Arnica latifolia, Goodyera oblongifolia, Viola orbiculata, and Orthilia secunda are the only forbs approaching or exceeding 50% constancy.
Diagnostic Characteristics: No Data Available
Rationale for Nominal Species or Physiognomic Features: No Data Available
Classification Comments: This very extensive and abundant association is slightly changed in name and concept from several pre-existing syntaxa. This association bears the dual designation for the tree canopy because this in fact describes over 95% of existing stand conditions with dominance shared by either or both species (Abies lasiocarpa or Picea engelmannii). When either or both of these species comprise less than 25% of the uppermost tree canopy cover, then another association is indicated. This association is very similar to or identical with Abies lasiocarpa / Rhododendron albiflorum / Xerophyllum tenax (Williams et al. 1995); only Rhododendron albiflorum needs to be added as a co-diagnostic species of the tall-shrub layer (with Menziesia ferruginea). In a few cases Rhododendron albiflorum is the sole dominant of this shrub layer, but this fact does not perceptibly change the environmental parameters defining this type. The addition of Rhododendron albiflorum to the key would create an overarching type extending from Banff and Jasper south to central Idaho. It is suggested that individual indicator shrub species or their combined cover need to be 5% or greater to recognize the type described here. Xerophyllum tenax must also exhibit at least 5% cover; it has been added to the type name so as to distinguish this association from others characterized by Menziesia ferruginea and Rhododendron albiflorum dominance. These other associations represent yet more extreme environments.
Similar NVC Types: No Data Available
note: No Data Available
Physiognomy and Structure: No Data Available
Floristics: This is a closed forest type for the most part with total upper canopy cover ranging upward from 60%. A variable mix of Abies lasiocarpa and Picea engelmannii dominate the canopy as well as the regeneration layers. Seral tree species do poorly on these sites; Pinus contorta, Pseudotsuga menziesii, and Larix occidentalis are the only tree species consistently present and seldom is their canopy cover as great as 20%. The modal condition for the undergrowth varies with geographic region; in northern Idaho and eastern Washington Menziesia ferruginea, joined by Rhododendron albiflorum in over half the stands inventoried, forms a lush and mostly continuous, tall (to 6 feet or more) shrub layer. This is contrasted with the physiognomy of stands on the east side of the Continental Divide where the tall-shrub canopy can be decidedly discontinuous and seldom exceeds 3-4 feet in height and lacks Rhododendron albiflorum, though Alnus viridis ssp. sinuata (= Alnus sinuata) and Sorbus scopulina are consistently present. In all parts of the type''s range Vaccinium membranaceum is the mid (short) shrub dominant with coverages generally upwards of 30%; it is usually accompanied by low cover of Ribes lacustre and the somewhat shorter Vaccinium scoparium (or its ecological analogue Vaccinium myrtillus). The only graminoid consistently present, Luzula glabrata, occurs in slightly greater than trace amounts in stands at higher elevations and experiencing deeper snowpack. The herb layer, depauperate in comparison to that of ~Abies lasiocarpa - Picea engelmannii / Menziesia ferruginea / Clintonia uniflora Forest (CEGL005893)$$, is strongly dominated by Xerophyllum tenax; Arnica cordifolia, Arnica latifolia, Goodyera oblongifolia, Viola orbiculata, and Orthilia secunda are the only forbs approaching or exceeding 50% constancy.
Dynamics: No Data Available
Environmental Description: This association occurs throughout the middle to northern Rocky Mountains and on into the Canadian Rockies of southwestern and west-central Alberta as a small- to large-patch type from mid to upper subalpine habitats. In the southerly portions of its distribution, the Wallowa and Seven Devils mountains and Idaho Batholith (somewhat disjunct in Teton Range of Wyoming), it faithfully occupies moderate to steep slopes of northerly aspects at elevations ranging from 1700 to 2195 m (5600-7200 feet), but dropping to 1370 m (4500 feet) where frost pocket conditions obtain. Further to the north it also occurs predominantly on northerly exposures, but at higher elevations in wetter climates, it may be found on western and even southern exposures; it can occur on a given slope from the toe, up the backslope to the slope shoulder, and in wetter climates is found on ridgetops as well. It is perhaps most widely distributed in western Montana where individual stands may comprise hundreds to thousands of acres. In a circumscribed area, such as Glacier National Park, it may have a fairly consistent elevational range of 1000 to 1200 m (5400-6600 feet). It exhibits no particular substrate preferences being found on granitics, fine-grained sedimentaries (including argillite and limestone), metasediments, and mica-schist; volcanic ash caps of varying depths (to 50 cm thickness) are very prevalent in the southern and western portions. The predominant soil texture is silt loam, and soils, at least those occurring in the U.S., are uniformly well-drained; in the Canadian Rockies soils are cited to be strongly developed podzols developed on morainal and colluvium (Ogilvie 1962, Achuff et al. 2002a) and Brunisols (Achuff et al. 2002a). Rock content of surface horizons ranges from about 15% to over 50%.
Geographic Range: This association occurs from the northernmost middle Rocky Mountains, throughout the northern Rocky Mountains and on into the Canadian Rockies at least to the latitude of Jasper National Park (Canada) as a small- to large-patch type from mid to upper subalpine habitats.
Nations: CA,US
States/Provinces: AB, ID, MT, OR, WA
Plot Analysis Summary:
http://vegbank.org/natureserve/ELEMENT_GLOBAL.2.730842
Confidence Level: Moderate
Confidence Level Comments: No Data Available
Grank: G4G5
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.5 Subalpine Fir - Engelmann Spruce - Whitebark Pine Rocky Mountain Forest Macrogroup | M020 | 1.B.2.Nb.5 |
Group | 1.B.2.Nb.5.c Engelmann Spruce - Subalpine Fir - Mountain Hemlock Moist Forest & Woodland Group | G218 | 1.B.2.Nb.5.c |
Alliance | A3614 Subalpine Fir - Engelmann Spruce Rocky Mountain Moist Forest Alliance | A3614 | 1.B.2.Nb.5.c |
Association | CEGL005895 Subalpine Fir - Engelmann Spruce / Rusty Menziesia / Common Beargrass Forest | CEGL005895 | 1.B.2.Nb.5.c |
Concept Lineage: This association (CEGL000307) was based on a Habitat Type concept, including the phases of the H.T. in this association. Phases of the H.T. have now been split out into association elements, as well as the seral components of the H.T.
Predecessors: No Data Available
Obsolete Names: No Data Available
Obsolete Parents: No Data Available
Synonomy: = Abies lasiocarpa - Picea engelmannii / Menziesia ferruginea / Xerophyllum tenax Forest (Hop et al. 2007)
< Abies lasiocarpa / Menziesia ferruginea Habitat Type (Pfister et al. 1977)
< Abies lasiocarpa / Menziesia ferruginea Habitat Type (Daubenmire and Daubenmire 1968)
< Abies lasiocarpa / Menziesia ferruginea Habitat Type (Steele et al. 1981)
< Abies lasiocarpa / Menziesia ferruginea Habitat Type (Steele et al. 1983)
>< Abies lasiocarpa / Menziesia ferruginea Habitat Type, Xerophyllum tenax Phase (Cooper et al. 1987)
< Abies lasiocarpa / Menziesia ferruginea Plant Association (Johnson and Simon 1987)
>< Abies lasiocarpa / Rhododendron albiflorum / Xerophyllum tenax Plant Association (Williams et al. 1995)
>< Picea engelmannii - Abies lasiocarpa / Menziesia ferruginea / Vaccinium membranaceum - Xerophyllum tenax Vegetation Type (Achuff et al. 2002)
>< Picea engelmannii - Abies lasiocarpa / Menziesia ferruginea Habitat Type (Ogilvie 1962)
>< Picea engelmannii - Pinus albicaulis / Menziesia glabella (= M. ferruginea) Vegetation Type (Holland and Coen 1982)
< Abies lasiocarpa / Menziesia ferruginea Habitat Type (Pfister et al. 1977)
< Abies lasiocarpa / Menziesia ferruginea Habitat Type (Daubenmire and Daubenmire 1968)
< Abies lasiocarpa / Menziesia ferruginea Habitat Type (Steele et al. 1981)
< Abies lasiocarpa / Menziesia ferruginea Habitat Type (Steele et al. 1983)
>< Abies lasiocarpa / Menziesia ferruginea Habitat Type, Xerophyllum tenax Phase (Cooper et al. 1987)
< Abies lasiocarpa / Menziesia ferruginea Plant Association (Johnson and Simon 1987)
>< Abies lasiocarpa / Rhododendron albiflorum / Xerophyllum tenax Plant Association (Williams et al. 1995)
>< Picea engelmannii - Abies lasiocarpa / Menziesia ferruginea / Vaccinium membranaceum - Xerophyllum tenax Vegetation Type (Achuff et al. 2002)
>< Picea engelmannii - Abies lasiocarpa / Menziesia ferruginea Habitat Type (Ogilvie 1962)
>< Picea engelmannii - Pinus albicaulis / Menziesia glabella (= M. ferruginea) Vegetation Type (Holland and Coen 1982)
- ANHIC [Alberta Natural Heritage Information Centre]. 2018. Community database files. Alberta Natural Heritage Information Centre, Parks and Protected Areas Division, Alberta Community Development, Edmonton.
- Achuff, P. L., R. L. McNeil, M. L. Coleman, C. Wallis and C. Wershler. 2002. Ecological land classification of Waterton Lakes National Park, Alberta. Volume I: Integrated resource description. Parks Canada, Waterton Lakes National Park, Alberta. 226 pp.
- 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. F., and J. B. Daubenmire. 1968. Forest vegetation of eastern Washington and northern Idaho. Washington State University Agricultural Experiment Station Technical Bulletin No. 60. 104 pp.
- Holland, W. D., and G. M. Coen, editors. 1982. Ecological (biophysical) land classification of Banff and Jasper national parks: Volume II, soil and vegetation resources. Publication No. SS-82-44. Alberta Institute of Pedology, Edmonton, AB. 540 pp.
- Hop, K., M. Reid, J. Dieck, S. Lubinski, and S. Cooper. 2007. U.S. Geological Survey-National Park Service Vegetation Mapping Program: Waterton-Glacier International Peace Park. U.S. Geological Survey, Upper Midwest Environmental Sciences Center, La Crosse, WI. 131 pp. plus Appendices A-L.
- 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.
- Ogilvie, R. T. 1962. Ecology of spruce forests on the east slope of the Rocky Mountains in Alberta. Unpublished dissertation, Washington State University, Pullman. 189 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.
- Reid, M. S., S. V. Cooper, and G. Kittel. 2004. Vegetation classification of Waterton-Glacier International Peace Park. Final report for USGS-NPS Vegetation Mapping Program, International Peace Park Mapping Project. NatureServe, Arlington VA.
- 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. V. Cooper, D. M. Ondov, D. W. Roberts, and R. D. Pfister. 1983. Forest habitat types of eastern Idaho - western Wyoming. General Technical Report INT-144. USDA Forest Service, Intermountain Forest and Range Experiment Station, Ogden, UT. 122 pp.
- Western Ecology Working Group of NatureServe. No date. International Ecological Classification Standard: International Vegetation Classification. Terrestrial Vegetation. NatureServe, Boulder, CO.
- Williams, C. K., B. F. Kelly, B. G. Smith, and T. R. Lillybridge. 1995. Forest plant associations of the Colville National Forest. General Technical Report PNW-GTR-360. USDA Forest Service, Pacific Northwest Region, Portland, OR. 140 pp.