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A1201 Calamovilfa longifolia - Andropogon hallii Sand Prairie Alliance

Type Concept Sentence: This alliance, found in the north Great Plains, occurs on sandy dry-mesic sites. Stands are almost exclusively found on sand deposits; a few are on coarse loams. There are two prominent vegetation layers in stands of this alliance and a moderate amount of bare ground. The tallest layer, about 0.6-1.5 m tall, is dominated by midgrasses, particularly Calamovilfa longifolia and Andropogon hallii.


Common (Translated Scientific) Name: Prairie Sandreed - Sand Bluestem Sand Prairie Alliance

Colloquial Name: Northern Plains Prairie Sandreed - Sand Bluestem Prairie

Hierarchy Level:  Alliance

Type Concept: This alliance, found in the northern Great Plains, occurs on sandy dry-mesic sites. There are two prominent vegetation layers in stands of this alliance and a moderate amount of bare ground. The tallest layer, about 0.6-1.5 m tall, is dominated by mid grasses, particularly Calamovilfa longifolia. Other species present include Andropogon hallii, Hesperostipa comata, Schizachyrium scoparium, Koeleria macrantha, and Sporobolus cryptandrus. The shorter layer includes several short graminoid species, forbs, and some small shrubs. Graminoids make up the majority of this layer, especially upland Carices. Among the most frequent are Carex duriuscula, Carex inops ssp. heliophila, and Carex filifolia. Bouteloua gracilis is prominent in some stands, especially in the western portion of this alliance''s range. Forbs and shrubs do not usually contribute greatly to the vegetation cover, although forb species diversity can be moderately high. The forbs that are present typically include Chenopodium leptophyllum, Lathyrus spp., Lygodesmia juncea, Phlox hoodii, and Liatris punctata. Psoralidium lanceolatum and Rumex venosus are most common on the least stabilized locations. Shrubs are uncommon, but when they are present, short shrubs such as Yucca glauca, Rosa spp., and Artemisia frigida are the most likely to be found. Artemisia cana and Elaeagnus commutata may be associated with more northern stands. Stands of this alliance are almost exclusively found on sand deposits; a few are on coarse loams. Stands are usually on gentle slopes but can be on flat ground or steep slopes. The soil is sand, loamy sand, or sandy loam, and there is little horizon development. Water penetrates the coarse soil quickly. This results in the upper soil having little available moisture for most of the growing season. Water and wind erosion can be frequent disturbances in this alliance.

Diagnostic Characteristics: These stands are on sandy soils throughout the northern Great Plains and are dominated by Calamovilfa longifolia and Andropogon hallii.

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: There is some overlap with ~Andropogon hallii Sand Prairie Alliance (A1193)$$ in those stands that contain both Andropogon hallii and Calamovilfa longifolia. All Calamovilfa gigantea populations in Nebraska are introduced (G. Steinauer, pers. comm. 2019), and it is absent from Wyoming and northeast Colorado. Calamovila longifolia and Andropogon hallii are important in eastern Colorado, but can be reduced leaving Hesperostipa comata dominated grasslands with heavy season long grazing. It can be reversed with light to moderate proper grazing (K. Decker, pers. comm. 2019).

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

Physiognomy and Structure: Vegetation included in this alliance has a moderate to dense herbaceous layer (0.5-1.5 m tall) that is dominated by tall grasses and mid grasses, with short grasses common in the western portion of its range. There is usually a sparse forb layer. Widely scattered low shrubs may also be present.

Floristics: Stands have a medium to tall herbaceous layer dominated by widely spaced bunchgrasses 0.6-1.5 m tall. This layer is dominated by Calamovilfa longifolia. Other species present include Achnatherum hymenoides (= Oryzopsis hymenoides), Andropogon hallii, Hesperostipa comata (= Stipa comata), Koeleria macrantha, Pascopyrum smithii (clayey sites), Schizachyrium scoparium, and Sporobolus cryptandrus. Many of these stands also have a second herbaceous layer dominated by short graminoid species, forbs, and some small shrubs. Graminoids make up the majority of this layer, especially upland Carex spp. Among the most frequent are Carex duriuscula (= Carex eleocharis, = Carex stenophylla), Carex inops ssp. heliophila, and Carex filifolia. Bouteloua gracilis is prominent in some stands, especially in the western portion of this alliance''s range. Forbs and shrubs do not usually contribute greatly to the vegetation cover, although forb species diversity can be moderately high (Hanson and Whitman 1938, USFS 1992). The forbs that are present typically include Artemisia spp., Chenopodium leptophyllum, Lathyrus spp., Liatris punctata, Lygodesmia juncea, and Phlox hoodii. Psoralidium lanceolatum and Rumex venosus are most common on the least stabilized locations. Shrubs are uncommon, but when they are present, short shrubs such as Artemisia filifolia, Artemisia frigida, Rhus trilobata, Rosa spp., and Yucca glauca are the most likely to occur.

Dynamics:  Wind is a dominant factor that shapes the landscape where this alliance occurs. Wind sometimes scours sand and vegetation from small areas and creates blowouts. These bare spots are initially colonized by species that are relatively uncommon in this alliance, such as Redfieldia flexuosa, Muhlenbergia pungens, Yucca glauca, and Achnatherum hymenoides. Eventually, these blowouts succeed to other communities (Savage 1937, Ramaley 1939b, Tolstead 1942, Harrison 1980). Tolstead (1942) cites Nebraska pioneer accounts that dunes were less vegetated than at present, and blowouts and stands were more common before cattle ranching. Fire frequency and extent are also thought to have declined since settlement because of fuel removal by livestock grazing and fire control (Burzlaff 1962, Wolfe 1973). Consequently, active dunes and large blowouts are less common now, as are the pioneer plant species Redfieldia flexuosa, Andropogon hallii, and Yucca glauca (Harrison 1980).

These grasslands provide excellent summer forage and need careful management to prevent grazing out desirable species. Generally, overgrazing this alliance decreases the cover of species of Andropogon, Calamovilfa, Eragrostis, and Hesperostipa, and increases the cover of Bouteloua gracilis, Bouteloua hirsuta, Muhlenbergia pungens, Achnatherum hymenoides, and Sporobolus cryptandrus (Savage 1937, Tolstead 1942, Harrison 1980). Overgrazing also kills out desirable shrubs, especially Amorpha canescens and Prunus pumila var. besseyi (Ryan et al. 1994). This grassland responds rapidly to management. Deferment of grazing in the late spring and summer favors warm-season grasses such as Andropogon hallii, Bouteloua hirsuta, Bouteloua gracilis, Calamovilfa longifolia, Eragrostis trichodes, Koeleria macrantha, and Schizachyrium scoparium.

Drought also causes declines in cover of all species, especially tall grasses, and can make the grassland more vulnerable to blowouts. Savage (1937) found large declines in tallgrass cover on sandy sites during drought in 1935. He ranked the cause of damage by decreasing effect: heat, drought, and, to a much lesser extent, grazing and then soil blowing. Ramaley (1939a, b) reports that in Colorado there is marginally enough precipitation to maintain this alliance. Drought causes retrogression to mixed sandhill, sand sage, or blowout communities, which increases Muhlenbergia pungens, Artemisia filifolia, and Achnatherum hymenoides. Grazing during droughts increases the intensity of the damage (Ramaley 1939a, b). Many of these stands, especially those disturbed by wind and grazing, are vulnerable to invasion by exotic annual species of Bromus such as Bromus arvensis, Bromus squarrosus, or Bromus tectorum (Comer et al. 1999).

Environmental Description:  Stands of this alliance occur on sandy sites in the central and northern Great Plains. The climate is temperate, continental with annual precipitation ranging from 46-61 cm. Elevations are generally between 1000 and 1600 m. Stands are found on stabilized sand dunes, interdune valleys, colluvial sand on toeslopes and badland benches (DeVelice et al. 1995). Sites where this alliance is found are usually on gentle to steep slopes on any aspect, but sometimes occur on flat ground (Tolstead 1942, Steinauer 1989). The soils are sand, loamy sand, or sandy loam, and they can be poorly to moderately well-developed (Looman 1980, Johnston 1987, Steinauer 1989). Parent materials include eolian sand and coarse-textured colluvium from sandstone, shales and other sedimentary rocks. There is little runoff or evaporation because moisture quickly sinks into the coarse soil. Soil near the surface is consequently dry throughout much of the year, but moisture is present deeper in the soil profile. This favors deep-rooting species such as Andropogon hallii and Calamovilfa longifolia (Barnes and Harrison 1982). Water and wind erosion can be frequent disturbances in this alliance. In the north and western extent, adjacent grasslands dominated by Pascopyrum smithii or Bouteloua spp. occur on fine-textured soils.

Geographic Range: Grasslands in this alliance occur on sandy sites in the northern Great Plains, including the sandhills of NE, Wyoming and north to Alberta, Saskatchewan and Manitoba, Canada.

Nations: CA,US

States/Provinces:  AB, MB?, MT, ND, NE, SD, SK, WY




Confidence Level: Low

Confidence Level Comments: No Data Available

Grank: GNR

Greasons: No Data Available


Concept Lineage: This alliance was not modified.

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: ? Calamovilfa longifolia Series (Johnston 1987) [Colorado]
? Bunchgrass Community (Weaver and Albertson 1956) [Nebraska]
? Postclimax Grasses on Dunes (Tolstead 1941) [South Dakota]
? Sand Prairie Community (Ramaley 1939a) [Colorado]
? Sand-hills Mixed Type (Weaver and Albertson 1956) [Colorado]
? Tall Grasses of the Dunes (Tolstead 1942) [Nebraska]
? USDA-NRCS Deep Sand Range Sites #15,16,19 (Soil Conservation Service 1978)

Concept Author(s): W.L. Tolstead (1942); J.E. Weaver and F.W. Albertson (1956)

Author of Description: S. Menard, K.A. Schulz, L. Allen

Acknowledgements: No Data Available

Version Date: 12-18-14

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