Print Report
A3735 Quercus gambelii - Symphoricarpos oreophilus Shrubland Alliance
Type Concept Sentence: This shrubland alliance of the Colorado Plateau and southern Rocky Mountains is characterized by dominance or codominance of Quercus gambelii in association with other mid-elevation shrubs.
Common (Translated Scientific) Name: Gambel Oak - Mountain Snowberry Shrubland Alliance
Colloquial Name: Gambel Oak - Mountain Snowberry Shrubland
Hierarchy Level: Alliance
Type Concept: This shrubland alliance occurs in the Colorado Plateau and southern Rocky Mountains and is characterized by dominance or codominance of Quercus gambelii in a moderately dense to dense tall- or short-shrub layer, typically 2-5 m tall, but can also occur as 1-m tall clumps to small trees over 5 m tall. The variable structure includes patches of oak shrubs with grass growing in between, dense oak thickets with little understory, and relatively mesic, tall shrublands with a rich understory of short shrubs, grasses and forbs. Scattered trees are occasionally present in stands and typically include species of Pinus or Juniperus. Characteristic shrubs that may codominate or form a separate short-shrub layer include Amelanchier alnifolia, Amelanchier utahensis, Artemisia tridentata, Cercocarpus montanus, Fendlera rupicola, Prunus virginiana, Rhus trilobata, Symphoricarpos oreophilus, and Symphoricarpos rotundifolius. The herbaceous layer is sparse to moderately dense, ranging from 1-40% cover and is dominated by perennial graminoids, particularly Bouteloua curtipendula, Bouteloua gracilis, Carex geyeri, Carex inops, Elymus arizonicus, Festuca thurberi, Koeleria macrantha, Muhlenbergia montana, Hesperostipa comata, and Poa fendleriana. Many forb and fern species can occur, but none has much cover. Stands occur in the foothills and lower montane slopes, mesas and canyons. Elevations range from 1550-2950 m. Sites range from nearly level mesatops to steep (to 80%), rocky slopes on upper slopes and ridgetops. Other stands occur in canyon bottoms and along drainages. Soils are generally deep, coarse-textured, and well-drained.
Diagnostic Characteristics: Temperate cold-deciduous shrublands 1-2 m tall dominated or codominated by Quercus gambelii in association with other mid-elevation shrubs. Understories are sparse to dense and typically grass- or sedge-dominated. Stands codominated by Robinia neomexicana are not included in this alliance.
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: Vegetation in this shrubland alliance is characterized by a moderately dense cover of broad-leaved deciduous shrubs. The graminoid layer is sparse to moderately dense and dominated by medium-tall bunchgrasses. The forb layer is generally sparse but may have high species diversity. Annual grasses and forbs are seasonally present.
Floristics: This shrubland alliance is characterized by dominance or codominance of Quercus gambelii in a moderately dense to dense tall- or short-shrub layer, typically 2-5 m tall, but can also occur as 1-m tall clumps to small trees over 5 m tall. The variable structure includes patches of oak shrubs with grass growing in between, dense oak thickets with little understory, and relatively mesic, tall shrublands with a rich understory of short shrubs, grasses and forbs. Scattered trees are occasionally present in stands and typically include Pinus edulis, Pinus ponderosa, or Juniperus spp. Characteristic shrubs that may codominate or form a separate short-shrub layer include Arctostaphylos patula, Amelanchier alnifolia, Amelanchier utahensis, Artemisia tridentata, Cercocarpus montanus, Fendlera rupicola, Holodiscus dumosus, Paxistima myrsinites, Ptelea trifoliata, Prunus virginiana, Rhus trilobata, Rosa spp., Symphoricarpos oreophilus, and Symphoricarpos rotundifolius. The herbaceous layer is sparse to moderately dense, ranging from 1-40% cover and is dominated by perennial graminoids, particularly Bouteloua curtipendula, Bouteloua eriopoda, Bouteloua gracilis, Carex geyeri, Carex inops, Elymus arizonicus, Festuca thurberi, Koeleria macrantha, Muhlenbergia montana, Hesperostipa comata, and Poa fendleriana. Many forb and fern species can occur, but none has much cover. Commonly present forbs include Achillea millefolium, Artemisia spp., Geranium spp., Maianthemum stellatum, Thalictrum fendleri, and Vicia americana. Ferns include species of Cheilanthes and Woodsia. Annual grasses and forbs are seasonally present. In Texas occurrences, associated species can include Holodiscus dumosus and Symphoricarpos oreophilus. Additional species found in associations of this alliance include Cercocarpus montanus, Carex geyeri, Amelanchier alnifolia, Amelanchier utahensis, Artemisia tridentata, Carex inops, Paxistima myrsinites, Rhus trilobata and Symphoricarpos rotundifolius.
Dynamics: The distribution of Quercus gambelii was studied by Neilson and Wullstein (1983) with respect to climatic patterns. They found the species to be limited by seedling mortality from severe spring frosts and summer drought. The northern extent of the species is in alignment with the winter polar front that runs along the boundary between southern Wyoming and Colorado and Utah. Its western range limit aligns with the westward extent of summer moisture from the Arizona monsoon, which approximates the western Arizona border. Reproducing stands in northern Utah that exist north of summer monsoon moisture are restricted to more mesic sites. Seedling recruitment is more common in the southern part of its range than the northern (Neilson and Wullstein 1983).
Quercus gambelii is a fire-adapted species (Clary 1992). The root systems are well-developed and draw moisture from a large volume of soil allowing for rapid resprouting after fire. Muldavin et al. (1998b) reported that, in the Organ Mountains in southwestern New Mexico after a severe fire, Quercus gambelii resprouted into a dense thicket that excluded both herbaceous understory and conifer species. They suggested frequent small cool fires would favor the establishment of conifers and maintain an herbaceous understory. Quercus gambelii shrubs also resprout vigorously after stems are killed with almost all herbicides or removed by chaining or cutting for firewood (Clary 1992). Altered fire regimes, fuelwood harvest, and grazing by livestock have significant impacts to the quality of sites. More study is needed to understand and manage these shrublands ecologically.
Quercus gambelii is a fire-adapted species (Clary 1992). The root systems are well-developed and draw moisture from a large volume of soil allowing for rapid resprouting after fire. Muldavin et al. (1998b) reported that, in the Organ Mountains in southwestern New Mexico after a severe fire, Quercus gambelii resprouted into a dense thicket that excluded both herbaceous understory and conifer species. They suggested frequent small cool fires would favor the establishment of conifers and maintain an herbaceous understory. Quercus gambelii shrubs also resprout vigorously after stems are killed with almost all herbicides or removed by chaining or cutting for firewood (Clary 1992). Altered fire regimes, fuelwood harvest, and grazing by livestock have significant impacts to the quality of sites. More study is needed to understand and manage these shrublands ecologically.
Environmental Description: Shrublands included in this alliance occur in the foothills and lower montane slopes of isolated desert mountain ranges, mesas and canyons from Nevada to western Texas, as well as in the lower montane zone of the southern Rocky Mountains, Uinta Mountains and high plateaus of southern Utah. Elevations range from 1550-2950 m. Climate is semi-arid. Summers are generally hot, and winters range from mild with cold periods and occasional snows in the southern part of its range to extended periods of freezing temperatures in the northern part of its range. The seasonality of precipitation varies, but most of the 35-70 cm of mean annual precipitation occurs during the growing season. Stands occur on nearly level to steep (to 80%), rocky slopes in canyons, mountain slopes and ridgetops while other stands occur in canyon bottoms and along drainages. Aspect does not seem important except in the southern range extent where stands are restricted to the more mesic north slopes. Soils are generally deep, coarse-textured, and well-drained. Soil texture is typically a cobbly and gravelly loamy sand and gravelly loam, but the alliance also occurs on well-drained clay soil. Parent materials are varied and include quartzite, monzonite, shale and alluvium. Adjacent vegetation at higher elevations is typically conifer woodlands or forests dominated by Pinus ponderosa, Pinus contorta, or Pseudotsuga menziesii, but Populus tremuloides forests are also common in the northern part of its range. Adjacent vegetation below these stands is often medium-tall grasslands in southeastern Colorado or shrublands dominated by Artemisia spp. in western Colorado.
Geographic Range: This alliance is known from the Colorado Plateau, southern Rocky Mountains, Great Basin, Utah High Plateaus, and Wyoming basins of Utah, Colorado, Wyoming, New Mexico and Arizona.
Nations: US
States/Provinces: AZ, CO, NM, TX, UT, WY
Plot Analysis Summary:
http://vegbank.org/natureserve/ELEMENT_GLOBAL.2.899787
Confidence Level: Moderate
Confidence Level Comments: No Data Available
Grank: GNR
Greasons: No Data Available
Concept Lineage: A.920 in large part
Predecessors: No Data Available
Obsolete Names: No Data Available
Obsolete Parents: No Data Available
Synonomy: = Quercus gambelii Association (132.111) (Brown 1982a) [included within Great Basin Montane Scrub, Oak-scrub Series]
= Quercus gambelii Series (Johnston 1987)
= Quercus gambelii Series (Johnston 1987)
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