Print Report

A3976 Pseudoroegneria spicata - Opuntia polyacantha Dry Canyon Slope Grassland Alliance

Type Concept Sentence: These dry grasslands occur in the canyons and valleys of the northern Great Basin and in the Columbia Basin and are characterized by a sparse to moderately dense graminoid layer of Pseudoroegneria spicata codominated by Aristida purpurea var. longiseta and/or Poa secunda. Pseudoroegneria spicata is sometimes absent or has low cover, and Sporobolus cryptandrus and Opuntia polyacantha may be especially abundant on disturbed or harsh windswept sites.


Common (Translated Scientific) Name: Bluebunch Wheatgrass - Plains Prickly-pear Dry Canyon Slope Grassland Alliance

Colloquial Name: Dry Canyon Slope Wheatgrass - Prickly-pear Grassland

Hierarchy Level:  Alliance

Type Concept: The vegetation of this dry grassland alliance is characterized by a sparse to moderately dense graminoid layer of Pseudoroegneria spicata codominated by Aristida purpurea var. longiseta and/or Poa secunda. Pseudoroegneria spicata is sometimes absent or has low cover. Sporobolus cryptandrus and Opuntia polyacantha are especially abundant on disturbed sites or harsh windswept ridgetops and steep upper slopes. Important forbs include Achillea millefolium, Allium acuminatum, Arnica sororia, Balsamorhiza sagittata, Castilleja spp., Calochortus spp., Crepis acuminata, Erigeron pumilus, Eriophyllum lanatum, Lupinus spp., Plantago patagonica, and Sedum stenopetalum. Deciduous shrubs such as Holodiscus discolor, Physocarpus malvaceus, Ribes spp., Rhus glabra, and Symphoricarpos spp. are occasionally present and may increase in abundance with fire exclusion. These grasslands occur in the canyons and valleys of the northern Great Basin and in the Columbia Basin, particularly along the Snake River canyon, the lower foothill slopes of the Blue Mountains, Wallowa Mountains, Hells Canyon, Seven Devil Mountains, and Salmon River Mountains of eastern Oregon, Washington and Idaho and along the main stem of the Columbia River in eastern Washington. Stands occur on gentle to steep mid and upper slopes and ridgetops in highly dissected foothills and canyon slope terrain and on stream terraces, alluvial fans, and benchlands in lower canyons. Sites are as low as 240 m and up to 1130 m elevation. Soils are typically shallow with a high percentage of rock fragments.

Diagnostic Characteristics: This alliance has a sparse to moderately dense graminoid layer characterized by diagnostic and often dominant species Pseudoroegneria spicata codominated by Aristida purpurea var. longiseta and/or Poa secunda. Pseudoroegneria spicata is sometimes absent or has low cover with Aristida purpurea var. longiseta and Poa secunda dominating. Indicator species Sporobolus cryptandrus and Opuntia polyacantha are especially abundant on disturbed sites or harsh windswept ridgetops and steep upper slopes.

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: These grasslands are floristically similar to other lower montane and foothill grasslands of the Central Rockies, but are found in environmental settings that tend to be drier than the "matrix" grasslands. Some of the dominant species (Aristida, Sporobolus, and Opuntia) are not particularly common in other Central Rockies grasslands, and forb taxa are also different.

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

Physiognomy and Structure: Vegetation in this alliance is characterized by a sparse to dense cover of graminoids that is dominated by perennial bunch grasses less than 1 m tall. There is also sparse to moderate cover of perennial forbs. Occasional scattered shrubs and dwarf-shrubs may be present. Annual forbs and grasses are seasonally present. Nonvascular cover is important in some stands.

Floristics: The vegetation is characterized by a sparse to moderately dense graminoid layer of Pseudoroegneria spicata codominated by Aristida purpurea var. longiseta and/or Poa secunda. Pseudoroegneria spicata is sometimes absent or has low cover. Sporobolus cryptandrus and Opuntia polyacantha are especially abundant on disturbed sites or harsh windswept ridgetops and steep upper slopes. Other associated grasses include Danthonia unispicata, Elymus elymoides, and Hesperostipa comata. Important forbs include Achillea millefolium, Allium acuminatum, Antennaria spp., Arnica sororia, Balsamorhiza sagittata, Castilleja spp., Calochortus spp., Crepis acuminata, Erigeron pumilus, Eriophyllum lanatum, Lomatium cous, Lupinus spp., Plantago patagonica, Scutellaria angustifolia, and Sedum stenopetalum. Deciduous shrubs such as Holodiscus discolor, Phlox longifolia, Physocarpus malvaceus, Ribes spp., Rhus glabra, and Symphoricarpos spp. are occasionally present and may increase in abundance with fire exclusion. The shrub Ericameria nauseosa (= Chrysothamnus nauseosus) is present in some stands, and will increase with overgrazing and other disturbance (Daubenmire 1970). The introduced annual grasses Bromus tectorum, Bromus arvensis (= Bromus japonicus), and Bromus briziformis and diverse non-native forbs such as Hypericum perforatum and Erodium cicutarium are abundant in many stands.

Dynamics:  Fire has variable effects on Pseudoroegneria spicata. Plants usually survive burning, and growth is often stimulated, except when fire occurs in the driest month when the crowns will burn because of low moisture in the vegetation, and the meristems are damaged (Johnson and Simon 1987). Grazing impacts are concentrated on the gentler slopes accessible to livestock. Pseudoroegneria spicata shows an inconsistent reaction to grazing, increasing on some grazed sites while decreasing on others. It seems to recover more quickly from overgrazing than Festuca campestris (Mueggler and Stewart 1980). It tolerates dormant-period grazing well, but is sensitive to defoliation during the growing season. Light spring use or fall grazing can help retain plant vigor. It is particularly sensitive to defoliation in late spring (Comer et al. 1999).

Poa secunda-dominated grasslands usually have relatively shallow, rocky soils with limited water-holding capacity. The winter precipitation wets these soils, but they typically dry out completely to bedrock by midsummer (Ganskopp 1979). Poa secunda is well-adapted to these conditions because it starts growing early in the spring and completes its reproductive cycle early while there is still moisture in the soil (Daubenmire 1970). If there is late summer or fall precipitation, dominant Poa secunda can green up quickly again. Shrubs are uncommon. Daubenmire (1970) and Johnson and Simon (1987) suggest that bedrock present under these grasslands is not fractured enough to support deeper-rooted shrubs. In addition to drought tolerance, Poa secunda is also tolerant of grazing and trampling by livestock (Daubenmire 1970, Ganskopp 1979).

Stands in this alliance are generally considered to be late-seral with species composition controlled by the harsh edaphic conditions of the site (Daubenmire 1970, Johnson and Simon 1987). However, some stands, especially stands of ~Aristida purpurea var. longiseta - Poa secunda Grassland (CEGL001781)$$ that occur on deeper soils, may be early-seral forms of a Pseudoroegneria spicata grassland, because Poa secunda increases under moderate grazing (Daubenmire 1970).

Sporobolus cryptandrus occurs throughout the western U.S. as a minor species, occasionally becoming locally dominant in disturbed or sandy sites in the midgrass prairie (Weaver and Albertson 1956). In the headwaters of the Columbia River basin these stands occur as climax grasslands in canyons on river bars and terraces, and on upland benches and terraces as grazing disclimax and edaphic climax grasslands (Daubenmire 1970, Johnson and Simon 1987, Tisdale 1986).

Many of these grasslands have been severely disturbed by grazing livestock and exotic weeds (Daubenmire 1970, Johnson and Simon 1987, Tisdale 1986). Early-season grazing reduces the abundance of the very palatable cool-season bunchgrass Pseudoroegneria spicata and favors the warm-season Sporobolus cryptandrus that greens up later in the season. Also, Sporobolus cryptandrus is a C4 plant that grows on sites that stay moist when it is hot, giving the C4 the advantage over the cool-season (C3) bunchgrasses. Poa secunda, another cool-season grass, is also affected by early grazing, but is better able to withstand it because of its short stature. Aristida purpurea var. longiseta is an unpalatable warm-season grass that increases as the palatable grasses decline. As native perennial grasses decline, exotic species fill the gaps (Tisdale 1986). Exotic annual grasses (Bromus tectorum, Bromus arvensis, and Bromus briziformis) and others may make up 20-50% of the vegetation cover. These annual grasses are especially abundant during wet years (Ganskopp 1979, Tisdale 1986).

Other disturbances such as frost heaving also favor exotic species invasion. Frost heaving causes local soil disturbance in the winter when these thin, saturated soils freeze and push soil and plants up out of the ground. Exotic forbs, both perennials such as Hypericum perforatum, and annuals such as Arenaria serpyllifolia, Epilobium brachycarpum, Erodium cicutarium, Draba verna, Holosteum umbellatum, Lactuca serriola, Lepidium perfoliatum, Myosotis stricta, Tragopogon dubius, and Veronica arvensis make up significant cover and diversity in many stands. The newest exotic threats are four species of Centaurea that are invading large areas in this region. Fire appears to have little effect on the species composition of these grasslands (Tisdale 1986).

Environmental Description:  These dry grasslands occur in the canyons and valleys of the northern Great Basin and in the Columbia Basin, particularly along the Snake River canyon, the lower foothill slopes of the Blue Mountains, Wallowa Mountains, Hells Canyon, Seven Devil Mountains, and Salmon River Mountains of eastern Oregon, Washington and Idaho and along the main stem of the Columbia River in eastern Washington. Climate is temperate continental. Mean annual precipitation ranges from 33-60 cm. Precipitation primarily occurs in the winter as snow or rain. Stands occur on gentle to steep mid and upper slopes and ridgetops in highly dissected foothills and canyon slope terrain and on stream terraces, alluvial fans, and benchlands in lower canyons. Sites are as low as 240 m and up to 1130 m elevation. This moisture is stored in the soil profile and utilized during the typically dry summers. Sites include soil pockets between rocks on cliffs lining the sides of ravines. This grassland occurs on all aspects, but is more common on southern slopes. Soils are typically shallow with a high percentage of rock fragments and exposed rock (lithic), but also may be moderately deep on some sites. They are moderately to well-drained, non-calcareous, sandy to clay soils with pH of 5.8-7.2, and are derived from alluvium, colluvium, residuum or loess. Parent materials include basalt, andesite, rhyolite and tuff. Rock and moss cover significant amounts of the ground surface often with over 40% cover of each.

Geographic Range: These dry grasslands occur in the canyons and valleys of the northern Great Basin and in the Columbia Basin, particularly along the Snake River canyon, the lower foothill slopes of the Blue Mountains, Wallowa Mountains, Hells Canyon, Seven Devil Mountains, and Salmon River Mountains of eastern Oregon, Washington and Idaho and along the main stem of the Columbia River in eastern Washington.

Nations: US

States/Provinces:  ID, NV, OR, WA




Confidence Level: Low

Confidence Level Comments: No Data Available

Grank: GNR

Greasons: No Data Available


Concept Lineage: This new alliance includes associations from Old Alliance V.A.5.N.d. Pseudoroegneria spicata Herbaceous Alliance (A.1265), Old Alliance V.A.5.N.d. Sporobolus cryptandrus Herbaceous Alliance (A.1252), Old Alliance V.A.5.N.h. Festuca idahoensis Alpine Herbaceous Alliance (A.1313), and Old Alliance V.A.5.N.f. Poa secunda Herbaceous Alliance (A.1291).

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: >< Agropyron spicatum Series (Johnson and Simon 1987)
>< Agropyron spicatum Series (Tisdale 1986)
>< Pseudoroegneria spicata Grasslands (Chappell et al. 1997)
>< Sporobolus cryptandrus - Aristida purpurea var. longiseta Grasslands (Chappell et al. 1997)
>< Bluebunch Wheatgrass - Sand Dropseed - Red Three Awn Plant Community Type - Sand (Johnson and Simon 1987)
= Bluebunch Wheatgrass Series (Johnson and Simon 1987) [roughly includes types in this alliance.]
>< Bluegrass Scabland (Volland 1976)
>< Bluegrass Scabland (Hall 1973)
>< River Terrace Canyon Grasslands (Kagan 1997)
? Sand Dropseed Plant Association (Johnson and Simon 1987)

Concept Author(s): C.G. Johnson and S.A. Simon (1987)

Author of Description: K.A. Schulz

Acknowledgements: This alliance is based in part on ~Columbia Basin Foothill and Canyon Dry Grassland (CES304.993)$$, ecological system concept (authored by R. Crawford, J. Kagan, and M. Reid).

Version Date: 09-21-15

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