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CEGL000618 Populus tremuloides / Tall Forbs Forest

Type Concept Sentence: No Data Available


Common (Translated Scientific) Name: Quaking Aspen / Tall Forbs Forest

Colloquial Name: No Data Available

Hierarchy Level:  Association

Type Concept: This Populus tremuloides forest is one of the most common and abundant aspen forest types in the Rocky Mountains. It occurs throughout mountainous areas and occurs on any aspect but tends to occur more often on north-facing slopes. It can be found on steep moist hillsides and often along narrow riparian areas. The broad-leaved deciduous tree canopy in dominated by Populus tremuloides. Low shrubs are virtually absent from this type. The undergrowth is characterized by a thick carpet of tall forbs (<1 m) with no one species dominant. Tall forbs include Agastache urticifolia, Delphinium x occidentale, Eucephalus engelmannii, Hackelia floribunda, Heracleum maximum, Mertensia arizonica, Osmorhiza occidentalis, Senecio serra, and Valeriana occidentalis. Other herbaceous species are present, including graminoid species. Forb species in streambank stands can be different from hillside stands.

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 vegetation of this type is structurally simple but may be compositionally complex. The canopy is dominated by Populus tremuloides, with occasional small amounts of conifer species present (particularly Abies lasiocarpa and Picea engelmannii). Shrubs are poorly represented, but Juniperus communis, Ribes sp., Sambucus racemosa, and Symphoricarpos oreophilus may occur with low cover. The herbaceous layer is characterized by the presence of several species of mesic tall forbs, accompanied by a mixture of low forbs and graminoids. The unifying characteristic of this type is the presence and usual prominence of one or more members of the tall-forb group of species, the absence of distinct shrub layers, and a lack of substantial amounts of conifers in the tree layer. Members of the tall-forb guild are Agastache urticifolia, Delphinium x occidentale, Eucephalus engelmannii (= Aster engelmannii), Hackelia floribunda, Heracleum maximum (= Heracleum lanatum), Mertensia arizonica, Osmorhiza occidentalis, Senecio serra, and Valeriana occidentalis (Mueggler 1988). No one member of this group is consistently dominant or even present, but as a group they form the dominant cover of the herbaceous layer, often exceeding 10%. Additional low forbs may include Achillea millefolium var. occidentalis (= Achillea lanulosa), Galium boreale, Galium triflorum, Geranium richardsonii, Geranium viscosissimum, Helianthella quinquenervis, Hydrophyllum fendleri, Ligusticum filicinum, Maianthemum stellatum, Streptopus amplexifolius, Thalictrum fendleri, Urtica dioica, and Viola spp. Common graminoids include Bromus spp., Calamagrostis canadensis, Carex spp., Elymus glaucus, and Poa pratensis. At higher elevations, with cooler conditions, Powell (1988a) describes two stands of this community type with Elymus glaucus dominating, which otherwise are floristically the same as described here. Many of the stands of this type are species-rich, and cover of the herbaceous understory is very high, usually over 200%.

Dynamics:  Successionally, this community type appears to be stable and, therefore, near climax (Mueggler 1988, Powell 1988a). Aspen is regenerating in some of the stands reported, while conifer regeneration is very low. The primary source of disturbance for this community is livestock grazing, which can have severe impacts. Species diversity will decrease, and palatable tall forbs may be eliminated with a shift in species composition to dominance by unpalatable forbs, such as Lathyrus and Rudbeckia spp. Extreme cases of abusive grazing, by either sheep or cattle, may result in a species-poor community, dominated by annuals (Mueggler 1988). Livestock may also significantly impact the growth of aspen shoots, impeding regeneration (Johnston and Hendzel 1985). Additional disturbance may be caused by timbering operations, which will adversely impact the wet soils of this type.

Fire is important to the initiation of these stands. The layer of tall forbs may help to carry fires, particularly during the dry fall season. Light fires will stimulate aspen suckering but may also kill the canopy trees.

Environmental Description:  This deciduous forest association occurs in the southern and central Rocky Mountains and plateaus and mountains of the Colorado Plateau and extends into the Jarbridge and Independence mountains of northeastern Nevada and into southwestern Montana. Stands occupy flat to gently sloping, moist to wet sites, often adjacent to streams. Slope positions are topographically low-lying, such as toeslopes or lower sidehills, flats, valley bottoms, and stream terraces. It is generally found on concave landforms where moisture can accumulate, rarely on convex topography. Aspect is variable, but many easterly or northerly stands are reported in the literature. Elevations are upper montane to lower subalpine and range from about 2100-3080 m (7000-10,000 feet), with most examples reported above 2745 m (9000 feet). Soils underlying this community type are derived from alluvial deposition of a variety of parent materials, but rarely is it found on volcanic soils (Mueggler 1988). The soils are deep, well-drained loams, sandy loams to clay loams in texture (Boyce 1977, Hess and Wasser 1982). With increasing depth, coarse and rock fragments increase in proportion. Hess and Wasser (1982) report very thin litter layers, and Boyce (1977) reports a low percentage of organic matter in the A horizon. Litter and duff comprise the majority of the unvegetated ground cover.

Geographic Range: This deciduous forest association occurs in the southern and central Rocky Mountains and plateaus and mountains of the Colorado Plateau and extends into the Jarbridge and Independence mountains of northeastern Nevada and into southwestern Montana.

Nations: US

States/Provinces:  CO, ID, MT, NV, UT, WY




Confidence Level: Moderate

Confidence Level Comments: No Data Available

Grank: G5

Greasons: No Data Available


Concept Lineage: No Data Available

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: ? Populus tremuloides / Elymus glaucus Plant Association (Powell 1988a)
= Populus tremuloides / Heracleum lanatum Community Type (Youngblood and Mueggler 1981)
= Populus tremuloides / Heracleum lanatum Community Type (Mueggler and Campbell 1982)
= Populus tremuloides / Ligusticum filicinum Community Type (Youngblood and Mueggler 1981)
= Populus tremuloides / Rudbeckia occidentalis Community Type (Mueggler and Campbell 1982)
= Populus tremuloides / Rudbeckia occidentalis Community Type (Youngblood and Mueggler 1981)
= Populus tremuloides / Senecio serra Community Type (Mueggler and Campbell 1982)
= Populus tremuloides / Tall Forb Community Type (Mueggler 1988)
= Populus tremuloides / Tall Forb Forest (Carsey et al. 2003a)
= Populus tremuloides/Tall forb (Kittel et al. 1999b)
= Quaking Aspen / Tall Forbs Forest (Populus tremuloides / Tall Forbs Forest) (Bell et al. 2009)
= Quaking aspen/tall forb (Populus tremuloides/Tall Forbs) Plant Association (Kittel et al. 1999a)
= Quaking aspen/tall forb (Populus tremuloides/tall forb) Plant Association (Kittel et al. 1997a)

Concept Author(s): M.S. Reid

Author of Description: M.S. Reid, G. Kittel and K.A. Schulz

Acknowledgements: No Data Available

Version Date: 01-10-06

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