Print Report

CEGL005877 Phyllodoce glanduliflora / Sibbaldia procumbens Dwarf-shrubland

Type Concept Sentence: No Data Available


Common (Translated Scientific) Name: Yellow Mountain-heath / Creeping Sibbaldia Dwarf-shrubland

Colloquial Name: No Data Available

Hierarchy Level:  Association

Type Concept: Documented from Glacier National Park, Montana. This community is found as small patches from the upper subalpine to alpine environments, its documented elevation range being from 1930 to 2320 m (6330-7610 feet). It is a moderately chionophilous type often noted as a dark green ericaceous border around long-persisting snowbed depressions. It also occurs on somewhat exposed ridges of terraced landscapes on positions where the ericaceous dwarf-shrubs are projecting through the snow in late June and July and the lower, less exposed positions in the landscape are still snow covered. It occurs on gentle terrain with slopes mostly less than 15% and noted to not exceed 35%. The accumulated peat layer is hypothesized to isolate the ericaceous root mat from differences in rock chemistry; therefore the community is found on both calcareous limestones and non-calcareous siltstones and argillites. The amount of exposed rock (which is frost-heaved to the surface) and soil is generally less than 5%, whereas litter in combination with moss and lichen cover form a nearly continuous cover. The heath species Phyllodoce glanduliflora, Phyllodoce empetriformis, and/or their hybrid Phyllodoce x intermedia, having at least 10% cover, are diagnostic for this community. In general the cover of these dwarf-shrubs exceeds 25% and they form a discontinuous layer about 0.15 m high. Salix arctica and Kalmia microphylla are the only other dwarf-shrubs of note. Carex nigricans is the one graminoid consistently present, though cover seldom exceeds 10%. Other high constancy graminoids include Phleum alpinum, Luzula glabrata, and a variable combination of Juncus species, Juncus mertensianus, Juncus drummondii, and Juncus parryi. Though its cover seldom exceeds 5%, Sibbaldia procumbens is diagnostic of the chionophilous nature of this community; other high-constancy forbs include Erigeron peregrinus, Packera streptanthifolia, Hieracium gracile, Arenaria capillaris, Hypericum scouleri, and Veronica wormskjoldii.

Diagnostic Characteristics: No Data Available

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: No Data Available

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

Physiognomy and Structure: No Data Available

Floristics: The heath species Phyllodoce glanduliflora, Phyllodoce empetriformis, and/or their hybrid Phyllodoce x intermedia, having at least 10% cover, are diagnostic for this community. In general the cover of these dwarf-shrubs exceeds 25% and they form a discontinuous layer about 0.15 m high. Salix arctica and Kalmia microphylla are the only other dwarf-shrubs of note. Carex nigricans is the one graminoid consistently present, though cover seldom exceeds 10%. Other high constancy graminoids include Phleum alpinum, Luzula glabrata, and a variable combination of Juncus species, Juncus mertensianus, Juncus drummondii, and Juncus parryi. Though its cover seldom exceeds 5%, Sibbaldia procumbens is diagnostic of the chionophilous nature of this community; other high-constancy forbs include Erigeron peregrinus, Packera streptanthifolia (= Senecio cymbalarioides), Hieracium gracile, Arenaria capillaris, Hypericum scouleri (= Hypericum formosum), and Veronica wormskjoldii.

Dynamics:  No Data Available

Environmental Description:  This community is found as small patches from the upper subalpine to alpine environments, its documented elevation range being from 1930 to 2320 m (6330-7610 feet). It is a moderately chionophilous type often noted as a dark green ericaceous border around long-persisting snowbed depressions. It also occurs on somewhat exposed ridges of terraced landscapes on positions where the ericaceous dwarf-shrubs are projecting through the snow in late June and July and the lower, less exposed positions in the landscape are still snow covered. It occurs on gentle terrain with slopes mostly less than 15% and noted to not exceed 35%. The accumulated peat layer is hypothesized to isolate the ericaceous root mat from differences in rock chemistry; therefore the community is found on both calcareous limestones and non-calcareous siltstones and argillites. The amount of exposed rock (which is frost-heaved to the surface) and soil is generally less than 5%, whereas litter in combination with moss and lichen cover form a nearly continuous cover.

Geographic Range: Documented from Glacier National Park, Montana.

Nations: CA,US

States/Provinces:  AB, MT




Confidence Level: Low

Confidence Level Comments: No Data Available

Grank: G2G3

Greasons: No Data Available


Concept Lineage: No Data Available

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: = Phyllodoce glanduliflora / Sibbaldia procumbens (Allen 2005)
= Phyllodoce glanduliflora / Sibbaldia procumbens Dwarf-shrubland (Hop et al. 2007)
< Sibbaldio procumbentis - Phyllodocetum glanduliflorae Association (Damm 2001)

Concept Author(s): Hop et al. (2007)

Author of Description: S.V. Cooper

Acknowledgements: No Data Available

Version Date: 01-13-04

  • Allen, L. 2005. Alberta Natural Heritage Information Centre Preliminary Plant Community Tracking List. Alberta Community Development, Edmonton, Alberta. 94 pp.
  • Allen, L. 2012-2013. Alberta Conservation Information Management System Ecological Community Tracking List. Alberta Tourism, Parks and Recreation, Edmonton, AB. [http://tpr.alberta.ca/parks/heritageinfocentre/default.aspx]
  • Damm, C. 2001. A phytosociological study of Glacier National Park, Montana, U. S. A., with notes on the syntaxonomy of alpine vegetation in western North America. Dissertation from Georg - August University, Germany. 297 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.
  • 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.
  • Western Ecology Working Group of NatureServe. No date. International Ecological Classification Standard: International Vegetation Classification. Terrestrial Vegetation. NatureServe, Boulder, CO.