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CEGL002490 Pinus banksiana - (Quercus ellipsoidalis) / Schizachyrium scoparium - Prairie Forbs Woodland
Type Concept Sentence: No Data Available
Common (Translated Scientific) Name: Jack Pine - (Northern Pin Oak) / Little Bluestem - Prairie Forbs Woodland
Colloquial Name: Jack Pine / Prairie Forbs Barrens
Hierarchy Level: Association
Type Concept: This jack pine barrens type is found in the northern tallgrass and prairie-forest border region of the United States and Canada. The topography is flat to rolling, and stands are formed on sands of glacial, lacustrine, or riverine origin. The sandy soils are acidic, droughty, and infertile. The open vegetation was historically influenced by fires. The vegetation is dominated by grasses and forbs with a sparse tree layer. The dominant tree is Pinus banksiana, with varying amounts of Quercus ellipsoidalis, Pinus resinosa, Populus tremuloides, and Populus grandidentata. The composition of all the strata of this community can vary significantly. Pinus banksiana is a constant across all sites, but it can be virtually the only tree species present or one of many. Quercus ellipsoidalis or Quercus macrocarpa can outnumber Pinus banksiana on some sites, especially those that have not been burned for many years. Pinus resinosa is typically at low densities in most examples of this community. Dry sites tend to have fewer woody shrub species and more herbaceous species with sand prairie affinities. Among these are Dalea villosa, Koeleria macrantha, Prunus pumila, Schizachyrium scoparium, and Calamovilfa longifolia. Dry-mesic areas have more Andropogon gerardii, Amorpha canescens, Liatris aspera, and Hesperostipa spartea. Patches of heath may occur, dominated by shrubby species such as Arctostaphylos uva-ursi, Comptonia peregrina, Hudsonia tomentosa, and Vaccinium angustifolium.
Diagnostic Characteristics: No Data Available
Rationale for Nominal Species or Physiognomic Features: No Data Available
Classification Comments: This community has a well-developed sand prairie flora, which may be a distinguishing feature separating it from ~Pinus banksiana - Pinus resinosa - (Quercus ellipsoidalis) / Carex pensylvanica Wooded Grassland (CEGL005124)$$, in eastern Wisconsin and Michigan. Further study is needed to resolve this issue. Frequently burned pine barrens sites can become scrubby, forming the ~Populus tremuloides - Quercus (ellipsoidalis, macrocarpa) / Andropogon gerardii Scrub Grassland (CEGL002197)$$. In low-lying areas, frost pockets can also contain this scrubby types.
Similar NVC Types: No Data Available
note: No Data Available
Physiognomy and Structure: This is a community with an open tree canopy, few woody shrubs, and extensive herbaceous ground cover. The density of trees as determined from General Land Office survey records was from 5-20 trees/ha on several sites in Wisconsin (Vogl 1961). It is very likely that more densely wooded examples of this community existed in the past as they can be seen currently in areas that have not been burned. At some level of canopy cover the site can no longer be classified as ~Pinus banksiana - (Quercus ellipsoidalis) / Schizachyrium scoparium - Prairie Forbs Wooded Herbaceous Vegetation (CEGL002490)$$ and is instead some type of woodland.
The density of the shrub layer appears to be related to the frequency of fire, the soil type, and the proximity of other, more closed forest types (Zimmerman 1956, MNNHP 1993). Sites close to the edge of extensive pine barrens have a more conspicuous shrub component. An increase in the fire interval also tends to allow more woody shrubs to proliferate. The density of the herbaceous layer is fairly constant, although some diminution of herbaceous cover occurs as the shrub layer becomes more closed. Tree canopy 10-20 m tall, short shrub 0.5-2 m and graminoid 0-2 m.
The density of the shrub layer appears to be related to the frequency of fire, the soil type, and the proximity of other, more closed forest types (Zimmerman 1956, MNNHP 1993). Sites close to the edge of extensive pine barrens have a more conspicuous shrub component. An increase in the fire interval also tends to allow more woody shrubs to proliferate. The density of the herbaceous layer is fairly constant, although some diminution of herbaceous cover occurs as the shrub layer becomes more closed. Tree canopy 10-20 m tall, short shrub 0.5-2 m and graminoid 0-2 m.
Floristics: The vegetation is dominated by grasses and forbs with a sparse tree layer. The dominant tree is Pinus banksiana, with varying amounts of Quercus ellipsoidalis, Pinus resinosa, Populus tremuloides, and Populus grandidentata. The composition of all the strata of this community can vary significantly. Pinus banksiana is a constant across all sites, but it can be virtually the only tree species present or one of many. Quercus ellipsoidalis or Quercus macrocarpa can outnumber Pinus banksiana on some sites, especially those that have not been burned for many years. Pinus resinosa is typically at low densities in most examples of this community. Dry sites tend to have fewer woody shrub species and more herbaceous species with sand prairie affinities. Among these are Dalea villosa, Koeleria macrantha, Prunus pumila, Schizachyrium scoparium, and Calamovilfa longifolia. Dry-mesic areas have more Andropogon gerardii, Amorpha canescens, Liatris aspera, and Hesperostipa spartea (= Stipa spartea). Patches of heath may occur, dominated by shrubby species such as Arctostaphylos uva-ursi, Comptonia peregrina, Hudsonia tomentosa, and Vaccinium angustifolium. Zimmerman (1956) also noted that stands of this community that are in the center of extensive sandplains have fewer deciduous tree species and shrubs.
The composition of all the strata of this community can vary significantly. Pinus banksiana is constant across all sites, but it can be virtually the only tree species present or one of many. Quercus ellipsoidalis can outnumber Pinus banksiana on some sites that have not been burned for many years. Pinus resinosa is typically at low densities in most examples of this community. Dry sites tend to have fewer woody shrub species and more herbaceous species with sand prairie affinities. Among these are Koeleria macrantha and Calamovilfa longifolia. Dry-mesic areas have more Andropogon gerardii, Amorpha canescens, and Hesperostipa spartea. Zimmerman (1956) also noted that stands of this community that are in the center of extensive sand plains have fewer deciduous tree species and shrubs. This community has scattered trees, little woody shrub component, and a fairly complete herbaceous cover. The dominant tree is Pinus banksiana, with varying amounts of Quercus ellipsoidalis, Pinus resinosa, and Populus spp. dominant in areas that have not been burned for many years. The shrub layer is more prominent near borders with other, more wooded communities. As the shrub layer increases there is some decrease in cover by the herbaceous layer.
The composition of all the strata of this community can vary significantly. Pinus banksiana is constant across all sites, but it can be virtually the only tree species present or one of many. Quercus ellipsoidalis can outnumber Pinus banksiana on some sites that have not been burned for many years. Pinus resinosa is typically at low densities in most examples of this community. Dry sites tend to have fewer woody shrub species and more herbaceous species with sand prairie affinities. Among these are Koeleria macrantha and Calamovilfa longifolia. Dry-mesic areas have more Andropogon gerardii, Amorpha canescens, and Hesperostipa spartea. Zimmerman (1956) also noted that stands of this community that are in the center of extensive sand plains have fewer deciduous tree species and shrubs. This community has scattered trees, little woody shrub component, and a fairly complete herbaceous cover. The dominant tree is Pinus banksiana, with varying amounts of Quercus ellipsoidalis, Pinus resinosa, and Populus spp. dominant in areas that have not been burned for many years. The shrub layer is more prominent near borders with other, more wooded communities. As the shrub layer increases there is some decrease in cover by the herbaceous layer.
Dynamics: Fire is the most important natural disturbance in this community, keeping the tree canopy very open. This community is maintained by relatively common surface fires. These fires suppress the growth of a dense shrub layer while leaving most of the relatively fire-resistant canopy trees intact. The droughty conditions and infertile soils of this community retard the development of the shrub layer even when fire is absent. Oaks, especially Quercus ellipsoidalis and Quercus macrocarpa, are present as grubs and scattered trees when fire is frequent. Oaks can become a common part of the canopy in the absence of fire. Fire is also necessary for the successful germination of the dominant trees, Pinus banksiana and Pinus resinosa. Pinus banksiana also needs fire to open its serotinous cones and allow the seeds to be spread. These species are not shade-tolerant, and fire clears out competing species which otherwise might shade these pines out. Fire frequency and intensity must allow some older trees to survive or else the site will become a grassland or brushland. Fire intervals of 20-40 years are thought to allow for successful regeneration of the dominant species without killing all of the older trees (Vogl 1970). More frequent fires can all but eliminate the pines. Other natural disturbances which contribute to maintaining the open nature of these barrens are windthrow and icestorms.
In most areas this community was successionally stable due to recurrent fires. In the absence of fires the canopy of this community will begin to close over and more shade-tolerant species will begin to invade. This has occurred on many former examples of this community. The process is greatly slowed by the infertile and excessively drained soils on which this community occurs. In northern Minnesota, Almendinger (1986) found jack pine barrens that form a transition phase as the forest invades prairie. The sparse tree physiognomy exists only on sites that have had Pinus banksiana on them for a few hundred years. This seral stage is quickly invaded by shrubs because of the rich Mollisols on which it occurs. The shrubs shade out the prairie flora and soon a different community develops.
In most areas this community was successionally stable due to recurrent fires. In the absence of fires the canopy of this community will begin to close over and more shade-tolerant species will begin to invade. This has occurred on many former examples of this community. The process is greatly slowed by the infertile and excessively drained soils on which this community occurs. In northern Minnesota, Almendinger (1986) found jack pine barrens that form a transition phase as the forest invades prairie. The sparse tree physiognomy exists only on sites that have had Pinus banksiana on them for a few hundred years. This seral stage is quickly invaded by shrubs because of the rich Mollisols on which it occurs. The shrubs shade out the prairie flora and soon a different community develops.
Environmental Description: This barrens community is found almost exclusively on dry, excessively drained, sandy soils (Vogl 1970, Almendinger 1986, Whitney 1986). This community may also occur as a relatively short-lived seral phase on richer Mollisols in Minnesota (Almendinger 1986). There it is quickly invaded by shrubs whose shade alters the community structure. The topography is usually flat to gently rolling, and stands are formed on sands of glacial, lacustrine, or riverine origin. The sandy soils are acidic, droughty, and infertile. This community occurs predominantly on glacial outwash or the sandy beds of former lakes. This community occurs almost exclusively over Entisols; some transient examples may be on Mollisols (Almendinger 1986). The Entisol soils are fine to coarse sands, sometimes loamy sands. These soils have poor nutrient-retaining capability due to the continuous presence of acidic pine litter during the Holocene, low concentrations of divalent cations in the parent material, and the sandy, well-drained character (Almendinger 1986). In Michigan, Zimmerman (1956) found all of the soils to be Grayling sands with a pH of 4.5-6.0. The droughtiness and inability of the soils to retain nutrients are the main environmental factors which maintain this community. Both factors exclude some species from existing in this community and they also reduce the productivity of those that do. The droughtiness also produces favorable conditions for fires to start and spread.
Geographic Range: This jack pine barrens type is found in the northern tallgrass and prairie-forest border region of the United States and Canada, ranging from southeastern Manitoba, the upper Mississippi River and St. Croix River in Minnesota, central Wisconsin and east to the High Plains of the interior of lower Michigan and in other scattered locations in upper Michigan.
Nations: CA,US
States/Provinces: MB, MI, MN, WI
Plot Analysis Summary:
http://vegbank.org/natureserve/ELEMENT_GLOBAL.2.688432
Confidence Level: Moderate
Confidence Level Comments: No Data Available
Grank: G2
Greasons: No Data Available
Type | Name | Database Code | Classification Code |
---|---|---|---|
Class | 1 Forest & Woodland Class | C01 | 1 |
Subclass | 1.B Temperate & Boreal Forest & Woodland Subclass | S15 | 1.B |
Formation | 1.B.2 Cool Temperate Forest & Woodland Formation | F008 | 1.B.2 |
Division | 1.B.2.Na Eastern North American Forest & Woodland Division | D008 | 1.B.2.Na |
Macrogroup | 1.B.2.Na.6 Eastern White Pine - Jack Pine - Northern Pin Oak Forest & Woodland Macrogroup | M159 | 1.B.2.Na.6 |
Group | 1.B.2.Na.6.d Jack Pine - Northern Pin Oak Barrens Group | G160 | 1.B.2.Na.6.d |
Alliance | A1499 Jack Pine - Pine species - Oak species Barrens Woodland Alliance | A1499 | 1.B.2.Na.6.d |
Association | CEGL002490 Jack Pine - (Northern Pin Oak) / Little Bluestem - Prairie Forbs Woodland | CEGL002490 | 1.B.2.Na.6.d |
Concept Lineage: No Data Available
Predecessors: No Data Available
Obsolete Names: No Data Available
Obsolete Parents: No Data Available
Synonomy: = Pinus banksiana - (Quercus ellipsoidalis) / Schizachyrium scoparium - Prairie Forbs Wooded Herbaceous Vegetation (Faber-Langendoen 2001) [Pine Barrens Jack Pine-Oak/Prairie Subtype]
= Jack Pine Barrens (MNNHP 1993)
= Jack Pine Barrens (MNNHP 1993)
- Almendinger, J. C. 1986. The natural history of the Paul Bunyan Arboretum. Unpublished paper. Department of Ecology and Behavioral Biology, University of Minnesota.
- Curtis, J. T. 1959. The vegetation of Wisconsin: An ordination of plant communities. Reprinted in 1987. University of Wisconsin Press, Madison. 657 pp.
- Faber-Langendoen, D., editor. 2001. Plant communities of the Midwest: Classification in an ecological context. Association for Biodiversity Information, Arlington, VA. 61 pp. plus appendix (705 pp.).
- Greenall, J. A. 1996. Manitoba''s terrestrial plant communities. MS Report 96-02. Manitoba Conservation Data Centre, Winnipeg.
- Kost, M. A., D. A. Albert, J. G. Cohen, B. S. Slaughter, R. K. Schillo, C. R. Weber, and K. A. Chapman. 2007. Natural communities of Michigan: Classification and description. Report No. 2007-21, Michigan Natural Features Inventory, Lansing. 314 pp. [http://web4.msue.msu.edu/mnfi/reports/2007-21_Natural_Communites_of_Michigan_Classification_and_Description.pdf]
- MNNHP [Minnesota Natural Heritage Program]. 1993. Minnesota''s native vegetation: A key to natural communities. Version 1.5. Minnesota Department of Natural Resources, Natural Heritage Program, St. Paul, MN. 110 pp.
- Midwestern Ecology Working Group of NatureServe. No date. International Ecological Classification Standard: International Vegetation Classification. Terrestrial Vegetation. NatureServe, Minneapolis, MN.
- Minnesota DNR [Minnesota Department of Natural Resources]. 2003-2005a. Field guide to the native plant communities of Minnesota. Three volumes: The Laurentian Mixed Forest Province (2003), The Eastern Broadleaf Forest Province (2005c), The Prairie Parkland and Tallgrass Aspen Parklands provinces (2005b). Ecological Land Classification Program, Minnesota County Biological Survey, and Natural Heritage and Nongame Research Program. Minnesota Department of Natural Resources, St. Paul.
- Minnesota DNR [Minnesota Department of Natural Resources]. 2003. Field guide to the native plant communities of Minnesota: The Laurentian Mixed Forest Province. Ecological Land Classification Program, Minnesota County Biological Survey, and Natural Heritage and Nongame Research Program. Minnesota Department of Natural Resources, St. Paul.
- Vogl, R. J. 1961. The effects of fire on some upland vegetation types. Ph.D. dissertation, University of Wisconsin. 103 pp.
- Vogl, R. J. 1964. Vegetational history of Crex Meadows, a prairie savanna in northwestern Wisconsin. The American Midland Naturalist 72(1):157-175.
- Vogl, R. J. 1970. Fire and the northern Wisconsin pine barrens. Proceedings of Tall Timbers Fire Ecology Conference 10:175-209.
- Vora, R. S. 1993. Moquah Barrens: Pine barrens restoration experiment initiated in Chequamegon National Forest. Restoration & Management Notes 11(1):39-44.
- WDNR [Wisconsin Department of Natural Resources]. 2015. The ecological landscapes of Wisconsin: An assessment of ecological resources and a guide to planning sustainable management. PUB-SS-1131 2015. Wisconsin Department of Natural Resources, Madison. [http://dnr.wi.gov/topic/landscapes/Book.html]
- Whitney, G. G. 1986. Relation of Michigan''s presettlement pine forests to substrate and disturbance history. Ecology 67(6):1548-1559.
- Whitney, G. G. 1987. An ecological history of the Great Lakes forest of Michigan. Journal of Ecology 75:667-684.
- Zimmerman, D. A. 1956. The jack pine association in the lower peninsula of Michigan: Its structure and composition. Ph.D. dissertation, University of Michigan.