Print Report

A3426 Juniperus osteosperma - Juniperus scopulorum / Shrub Understory Central Rocky Mountain Woodland Alliance

Type Concept Sentence: This foothill and outcrop alliance primarily occurs along the eastern slope of the central Rocky Mountains and adjacent Great Plains, but extends from central Colorado to Alberta. Stands have an open to moderately dense tree canopy dominated by Juniperus scopulorum or, less commonly, dominated by Juniperus osteosperma with understory characterized by an open to moderately dense shrub cover. Shrub cover is typically >10%, but if less, then shrub cover exceeds herbaceous layer.


Common (Translated Scientific) Name: Rocky Mountain Juniper - Utah Juniper / Shrub Understory Central Rocky Mountain Woodland Alliance

Colloquial Name: Central Rocky Mountain Juniper / Shrub Woodland

Hierarchy Level:  Alliance

Type Concept: This woodland alliance occurs in foothill and lower montane zones in the Rocky Mountains from southern Alberta and northern Montana south to central Colorado and on escarpments across Wyoming extending out into the western Great Plains. The vegetation is characterized by an open-tree canopy or patchy woodland that is dominated by either Juniperus scopulorum or, less commonly, Juniperus osteosperma. Pinus flexilis is absent or has low cover. The understory is characterized by open to moderately dense shrub cover (>10%) composed of Artemisia nova, Artemisia tridentata, Cercocarpus ledifolius, Cercocarpus montanus, or Purshia tridentata. Total shrub cover is typically >10%, but if less, then shrub cover exceeds herbaceous layer. These are rock outcrop, escarpment and patchy woodlands, occurring generally below continuous forests of Pseudotsuga menziesii or Pinus ponderosa. Elevation ranges from 1000-2400 m. Climatologically, the region is semi-arid and has a continental regime of hot summers and cold winters. Precipitation patterns are variable, but snow is common in winter, and spring rains are an important contributor. At higher elevations, it is limited to the most xeric aspects on rock outcrops, and at lower elevations to the relatively mesic north aspects. Slopes range from gentle to steep. Soils are typically thin, stony, clay or clay loam, commonly with exposed bedrock. The soil parent material varies with community association, but may be limestone, gneiss, sandstone, scoria, or shale. Stands area best developed on calcareous soils.

Diagnostic Characteristics: The alliance includes stands of patchy woodlands found on rock outcrops and escarpments at foothill elevations along the eastern Rocky Mountains Front Range out into the western Great Plains. Dominant and characteristic species are Juniperus scopulorum and Juniperus osteosperma. Shrubs characterize the understory with low to moderately dense cover. This alliance includes stands with a sparse understory of scattered shrubs. Herbaceous cover is sparse to moderately dense, but has less cover than shrubs. Diagnostic understory species include widespread Interior West species such as Artemisia nova, Artemisia tridentata, Cercocarpus ledifolius, Cercocarpus montanus, Ericameria nauseosa, or Purshia tridentata.

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: Juniperus scopulorum is a wide-ranging species in the Rocky Mountains and may dominate stands in other groups. Juniperus osteosperma-dominated stands from the Pryor, Big Horn, and Laramie mountain ranges are included in this alliance because these stands are significantly disjunct from the main distribution of Juniperus osteosperma in the Colorado Plateau and Great Basin regions and have floristic similarities to the Great Plains. Tree canopy is typically 10-35% cover or more, but includes stands with 5-9% tree cover when trees characterize the stand on rocky outcrops, i.e., shrub cover is sparse and is less than tree cover.

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

Physiognomy and Structure: Vegetation included in this alliance has an open to moderately dense tree canopy that is typically 2-5 m tall. Stands are solely dominated by evergreen scale-leaved trees. Scattered evergreen needle-leaved or deciduous broad-leaved trees may be present, but they never codominate. A sparse to moderately dense shrub layer may be present as a mixture of broadleaf and microphyllous, deciduous or evergreen shrubs that are usually less than 2 m tall. A sparse to moderately dense herbaceous layer dominated by perennial graminoids is usually present. Perennial forbs may be scattered. Annual forbs and grasses may be seasonally present.

Floristics: This woodland alliance occurs in foothill and lower montane zones in the Rocky Mountains from southern Alberta and northern Montana south to central Colorado and on escarpments across Wyoming extending out into the western Great Plains. The vegetation is characterized by an open to closed tree canopy (typically 10-35% cover) or patchy woodland usually 2-8 m tall that is dominated by either Juniperus scopulorum or, less commonly, Juniperus osteosperma. Pinus flexilis is absent or has low cover. In the plains stands the deciduous broad-leaved tree Fraxinus pennsylvanica may be present. Higher elevations stands may have scattered individuals of Pinus ponderosa, or Pseudotsuga menziesii may be present with low cover (<5% cover). Although cover of trees is typically >10% in this alliance, stands with 5-9% tree cover are included when trees characterize the stand and cover of trees exceeds cover of understory layers. The understory is characterized by open to moderately dense short-shrub cover (usually 10-35%) but includes denser stands. The dominant shrub species are Artemisia nova, Artemisia tridentata, Cercocarpus ledifolius, Cercocarpus montanus, Prunus virginiana, and Purshia tridentata. Common, but less abundant shrubs include Ericameria nauseosa (= Chrysothamnus nauseosus), Physocarpus monogynus, Purshia tridentata, Rhus trilobata, Ribes spp., Rubus deliciosus, and Symphoricarpos spp. Scattered dwarf-shrubs such as Artemisia frigida or Linanthus pungens (= Leptodactylon pungens) are frequently present. Total shrub cover is typically >10%, but if less, then shrub cover exceeds herbaceous layer. The herbaceous layer is dominated by graminoids typical of dry habitats. These species include Achnatherum hymenoides (= Oryzopsis hymenoides), Bouteloua gracilis, Carex rossii, Festuca idahoensis, Leucopoa kingii (= Festuca kingii), Hesperostipa comata (= Stipa comata), Leymus ambiguus, Muhlenbergia montana, Piptatheropsis micrantha (= Oryzopsis micrantha), Poa secunda, Pseudoroegneria spicata, and Schizachyrium scoparium. Perennial forbs are sparse but may be fairly diverse. The most common forbs are Achillea millefolium, Artemisia ludoviciana, Campanula rotundifolia, Eriogonum umbellatum, Galium boreale, Helianthus pumilus, Heterotheca villosa, Heuchera bracteata, Maianthemum stellatum, Penstemon virens, Potentilla fissa, and Senecio integerrimus. The fern Cystopteris fragilis and the cactus Opuntia polyacantha are often present. In some stands mosses and lichens cover up to 72% of the ground surface. Annual grasses and forbs are seasonally present. Some stands in rocky terrain may lack an understory.

Dynamics:  Woodlands in this alliance are considered to be edaphic or topographic climax communities (Hansen et al. 1984, Tiedemann et al. 1987). Juniperus scopulorum is a long-lived species. Hansen and Hoffman (1988) found most trees in stands they sampled to be over 120 years, with some individuals older than 360 years. Fire can be used to control Juniperus scopulorum stands on rangeland because the species will not resprout after being burned (Wright et al. 1979, Fischer and Bradley 1987). Young individuals are most vulnerable to fire (Wright et al. 1979, Fischer and Bradley 1987). The effect of fire on a stand is largely dependent on the tree height and density, fine fuel load on the ground, weather conditions, and season (Wright et al. 1979). Trees are more vulnerable in open stands where fires frequently occur in the spring when the humidity is low, wind speeds are over 10-20 mph, and there is adequate fine fuels to carry fire (Wright et al. 1979, Fischer and Bradley 1987). Under other conditions, burns tend to be spotty with low tree mortality. Large trees are generally not killed unless fine fuels, such as tumbleweeds, have accumulated beneath the tree to provide fuel ladders for the fire to reach the crown. Closed-canopy stands rarely burn because they typically do not have enough understory or wind to carry a fire. Altered fire regimes, cutting trees for fencing, and improper grazing by livestock have significant impacts on the quality of sites. Grazing by livestock can modify the fire regime by removing the fine fuels that carry fire. Fire, livestock grazing, and trampling by hikers and vehicles disturb biological soil crusts that help maintain soil structure, reduce soil erosion, provide habitat for plants and preserve biological diversity. More study is needed to understand and manage these woodlands.

Environmental Description:  These are rock outcrop, escarpment and patchy woodlands, occurring generally below continuous forests of Pseudotsuga menziesii or Pinus ponderosa from the lower montane zone in the Rocky Mountains and Black Hills to breaks in the Great Plains. Elevation ranges from 1000-2400 m. Climatologically, the region is semi-arid and has a continental regime of hot summers and cold winters. Precipitation patterns are variable, but snow is common in winter, and spring rains are an important contributor. At higher elevations, it is limited to the most xeric aspects on rock outcrops, and at lower elevations to the relatively mesic north aspects. Slopes range from gentle to steep. Soils are typically thin, stony, clay or clay loam, commonly with exposed bedrock. The soil parent material varies with community association, but may be limestone, gneiss, granite, sandstone, scoria, or shale. Stands are best developed on calcareous soils. Exposed bedrock is common and many stands have over 50% bare soil. Soil pH ranges from slightly acidic to alkaline.

Adjacent vegetation at higher elevations is woodland and forest dominated by Pinus ponderosa, Pinus flexilis, or Pseudotsuga menziesii. Adjacent vegetation at lower elevations includes shrubland dominated by Artemisia spp., Cercocarpus spp., or Purshia tridentata, riparian woodland dominated by Pseudotsuga menziesii, or dry prairie. The transition can be abrupt or an extended ecotone where the woodland grades into a savanna.

Geographic Range: This alliance occurs in foothill and lower montane zones in the Rocky Mountains from southern Alberta and northern Montana south to central Colorado and on escarpments across Wyoming extending out into the western Great Plains.

Nations: CA,US

States/Provinces:  AB, CO, ID, MT, SD, UT, WY




Confidence Level: Moderate

Confidence Level Comments: No Data Available

Grank: GNR

Greasons: No Data Available


Concept Lineage: One association from Old Alliance II.A.4.N.a. Juniperus osteosperma Woodland Alliance (A.536) and several associations from Old Alliance II.A.4.N.a. Juniperus scopulorum Woodland Alliance (A.506) are included in this alliance. A.506 (in part)

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: > Juniperus osteosperma / Cercocarpus ledifolius Community Type (DeVelice and Lesica 1993)
> Juniperus scopulorum - Artemisia tridentata - Bouteloua gracilis Vegetation Type (Jennings 1979)
> Juniperus scopulorum - Cercocarpus ledifolius Community Type (DeVelice 1992)
> Juniperus scopulorum - Cercocarpus ledifolius Community Type (Cooper et al. 1995)
> Juniperus scopulorum / Agropyron spicatum Plant Association (DeVelice et al. 1995)
> Juniperus scopulorum / Artemisia nova Community Type (DeVelice and Lesica 1993)
> Juniperus scopulorum / Artemisia nova Community Type (Lesica and DeVelice 1992)
> Juniperus scopulorum / Artemisia tridentata Community Type (Cooper et al. 1995)
> Juniperus scopulorum / Artemisia tridentata Community Type (DeVelice 1992)
> Juniperus scopulorum / Artemisia tridentata Habitat Type (Wasser and Hess 1982)
> Juniperus scopulorum / Artemisia tridentata Habitat Type (Hess and Alexander 1986)
> Juniperus scopulorum / Artemisia tridentata Habitat Type (Hess 1981)
> Juniperus scopulorum / Cercocarpus montanus Habitat Type (Hess and Alexander 1986)
> Juniperus scopulorum / Cercocarpus montanus Habitat Type (Hess 1981)
> Juniperus scopulorum / Cercocarpus montanus Habitat Type (Wasser and Hess 1982)
> Juniperus scopulorum / Cercocarpus montanus Plant Association (Baker 1984a)
> Juniperus scopulorum / Purshia tridentata Habitat Type (Hess 1981)
> Juniperus scopulorum / Purshia tridentata Habitat Type (Hess and Alexander 1986)
> Juniperus scopulorum / Purshia tridentata Habitat Type (Wasser and Hess 1982)
< Juniperus scopulorum Series (Johnston 1987)
< Juniperus scopulorum Series (Hess 1981)
> Juniperus / mountain mahogany woodland (Knight et al. 1987)
> Utah Juniper - Curlleaf Mountain Mahogany Stand (Marriott and Jones 1989)

Concept Author(s): K.A. Schulz, in Faber-Langendoen et al. (2013)

Author of Description: K.A. Schulz

Acknowledgements: No Data Available

Version Date: 01-08-14

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