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CEGL000185 Pinus ponderosa / Festuca campestris Woodland

Type Concept Sentence: No Data Available


Common (Translated Scientific) Name: Ponderosa Pine / Rough Fescue Woodland

Colloquial Name: No Data Available

Hierarchy Level:  Association

Type Concept: This association is most prevalent throughout northwestern Montana and the isolated ranges of central Montana, but it also occurs farther west in northern Idaho, eastern Washington, and possibly in interior British Columbia. It occurs primarily as small (to large) stands on south- and west-facing slopes at elevations of less than 1525 m (5000 feet). It is also found on moderate north slopes and benchlands near lower timberline where it transitions to fescue grasslands or ~Pinus ponderosa / Pseudoroegneria spicata Woodland (CEGL000865)$$ on drier exposures. It occurs on a broad spectrum of parent materials, including calcareous substrates. Surface soils are generally gravelly, ranging from silts to fine sandy loams. Bare soil is minimal, and there are only moderate amounts of exposed rock. Soils average about 4 cm of duff depth and have a darkened A1 surface horizon, indicative of the strong influence of abundant graminoids and forbs on soil development. Stands are open to approaching a savanna-like condition and uniquely dominated by Pinus ponderosa with negligible amounts of Pinus flexilis and/or Juniperus scopulorum; Pseudotsuga menziesii is considered to be an "accidental." The shrub component is depauperate in species and cover, with only Amelanchier alnifolia and Symphoricarpos albus exhibiting constancy approaching 50%. Bunchgrasses dominate the undergrowth (highest coverages approaching 70%, averaging about 55%) with dominance shifting between Festuca campestris, Festuca idahoensis, Pseudoroegneria spicata, Koeleria macrantha, Elymus trachycaulus, Achnatherum occidentale, and Achnatherum nelsonii, depending on disturbance regime (livestock grazing primarily). Forbs of highest constancy include Achillea millefolium, Anemone multifida, Balsamorhiza sagittata, Lithospermum ruderale, Galium boreale, Geum triflorum, and Potentilla gracilis; total forb cover seldom exceeds 20%.

Diagnostic Characteristics: No Data Available

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: As described and documented by Pfister et al. (1977), this is a climax plant association (habitat type) at the dry end of the moisture gradient of sites capable of supporting tree-dominated vegetation. As originally conceived, Pinus ponderosa (and to a limited degree Pinus flexilis and Juniperus scopulorum) should be the only trees capable of establishing on such xeric sites. However, the International Vegetation Classification (IVC) recognizes no distinction between types defined by potential versus those representing existing vegetation, which means stands with other conifer species in the subcanopy or reproductive layers (most likely Pseudotsuga) will classify to this type until the more shade-tolerant species assume dominance.

Similar NVC Types: No Data Available
note: No Data Available

Physiognomy and Structure: No Data Available

Floristics: Stands are open to approaching a savanna-like condition and uniquely dominated by Pinus ponderosa with negligible amounts of Pinus flexilis and/or Juniperus scopulorum; Pseudotsuga menziesii is considered to be an "accidental." The shrub component is depauperate in species and cover, with only Amelanchier alnifolia and Symphoricarpos albus exhibiting constancy approaching 50%. Bunchgrasses dominate the undergrowth (highest coverages approaching 70%, averaging about 55%) with dominance shifting between Festuca campestris, Festuca idahoensis, Pseudoroegneria spicata, Koeleria macrantha, Elymus trachycaulus (= Agropyron caninum), Achnatherum occidentale (= Stipa occidentalis), and Achnatherum nelsonii (= Stipa nelsonii), depending on disturbance regime (livestock grazing primarily). Forbs of highest constancy include Achillea millefolium, Anemone multifida, Balsamorhiza sagittata, Lithospermum ruderale, Galium boreale, Geum triflorum, and Potentilla gracilis; total forb cover seldom exceeds 20%.

Dynamics:  No Data Available

Environmental Description:  This association is most prevalent throughout northwestern Montana and the isolated ranges of central Montana, but it also occurs farther west in northern Idaho, eastern Washington, and possibly in interior British Columbia. It occurs primarily as small (to large) stands on south- and west-facing slopes at elevations of less than 1525 m (5000 feet). It is also found on moderate north slopes and benchlands near lower timberline where it transitions to fescue grasslands or ~Pinus ponderosa / Pseudoroegneria spicata Woodland (CEGL000865)$$ on drier exposures. It occurs on a broad spectrum of parent materials, including calcareous substrates. Surface soils are generally gravelly, ranging from silts to fine sandy loams. Bare soil is minimal, and there are only moderate amounts of exposed rock. Soils average about 4 cm of duff depth and have a darkened A1 surface horizon, indicative of the strong influence of abundant graminoids and forbs on soil development.

Geographic Range: This association is most prevalent throughout northwestern Montana and the isolated ranges of central Montana but occurs farther west in northern Idaho and eastern Washington. It may also occur in interior British Columbia.

Nations: CA?,US

States/Provinces:  BC?, ID, MT, WA




Confidence Level: Low

Confidence Level Comments: No Data Available

Grank: G3G4

Greasons: No Data Available


Concept Lineage: No Data Available

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: = Pinus ponderosa / Festuca campestris Habitat Type (Pfister et al. 1977)

Concept Author(s): Western Ecology Group

Author of Description: S.V. Cooper

Acknowledgements: No Data Available

Version Date: 04-25-07

  • 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. 2003. Assessment of Kootenai National Forest vegetation types with potential for Silene spaldingii in the Tobacco Plains, Rexford Bench and Salish Range foothills. Unpublished report to Kootenai National Forest, Supervisor''s Office. Montana Natural Heritage Program, Helena, MT. 33 pp. plus appendices.
  • 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.
  • MTNHP [Montana Natural Heritage Program]. 2002b. List of ecological communities for Montana. Montana Natural Heritage Program, Montana State Library, Helena, MT.
  • MTNHP [Montana Natural Heritage Program]. No date. Unpublished data on file. Montana Natural Heritage Program, Helena, MT.
  • McLean, A. 1970. Plant communities of the Similkameen Valley, British Columbia, and their relationships to soils. Ecological Monographs 40(4):403-424.
  • 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.
  • WNHP [Washington Natural Heritage Program]. 2018. Unpublished data files. Washington Natural Heritage Program, Department of Natural Resources, Olympia, WA.
  • Western Ecology Working Group of NatureServe. No date. International Ecological Classification Standard: International Vegetation Classification. Terrestrial Vegetation. NatureServe, Boulder, CO.