Print Report
CEGL007208 Fagus grandifolia - Quercus alba / Ilex opaca / Athyrium filix-femina ssp. asplenioides Forest
Type Concept Sentence: No Data Available
Common (Translated Scientific) Name: American Beech - White Oak / American Holly / Southern Ladyfern Forest
Colloquial Name: West Gulf Coastal Plain Beech - White Oak Forest (Typic Type)
Hierarchy Level: Association
Type Concept: This mesic acidic forest of the West Gulf Coastal Plain is dominated by Fagus grandifolia and Quercus alba. It is further typified by the presence of a fairly diverse number of species which indicate high-quality mesic, acidic habitats in the region. The scattered to patchy tall-shrub stratum includes Ilex opaca var. opaca, Carpinus caroliniana, Ostrya virginiana, Cornus florida, Styrax grandifolius, and Crataegus marshallii. The sparse herbaceous layer includes Polystichum acrostichoides, Trillium gracile, Prenanthes altissima (uncommon), Spigelia marilandica (uncommon), Galium circaezans, Desmodium nudiflorum, Uvularia perfoliata, Polygonatum biflorum, Arisaema triphyllum, Viola walteri, Mitchella repens, Tipularia discolor, Lilium michauxii, Smilax herbacea (uncommon-rare), and Podophyllum peltatum.
Diagnostic Characteristics: No Data Available
Rationale for Nominal Species or Physiognomic Features: No Data Available
Classification Comments: This type may include a number of understory species which become quite rare in the western part of the region, e.g., Sanguinaria canadensis and Uvularia perfoliata [see Kral (1966), Orzell (1990)]. The inclusion of Magnolia acuminata in this type is quite interesting given the narrow range of this species in the region. It is apparently rare in the Arkansas portion of the region (Smith 1988a) and is not found at all in Texas (Hatch et al. 1990). This type is present at the Beech Creek site in southern Arkansas (T. Foti pers. comm. 2001)
Similar NVC Types: No Data Available
note: No Data Available
Physiognomy and Structure: No Data Available
Floristics: Stands are dominated by a combination of Fagus grandifolia and Quercus alba (NatureServe Ecology unpubl. data, Turner et al. unpubl. data). Some stands may have slightly more Quercus alba than Fagus grandifolia and vice versa (R. Evans pers. obs.). Pinus taeda may occur in the canopy but not as a dominant. Although Fagus grandifolia and Quercus alba may be the only canopy species in some occurrences, canopy species in other occurrences may include Quercus michauxii, Quercus pagoda, Quercus velutina, Quercus nigra, Quercus stellata, Carya tomentosa (= Carya alba), Nyssa sylvatica, Liquidambar styraciflua, and Acer rubrum. Liriodendron tulipifera may be present in Arkansas and Louisiana examples, but is not a natural component of this type in Texas or Oklahoma. Magnolia grandiflora may also be present in examples of this type in Louisiana and Texas, but is absent in Arkansas and Oklahoma. Phoradendron leucarpum, Tillandsia usneoides, and Pleopeltis polypodioides (= Polypodium polypodioides) are common epiphytes on the canopy trees. The scattered to patchy tall-shrub stratum includes regenerating canopy species and Ilex opaca var. opaca, Carpinus caroliniana, Ostrya virginiana, Cornus florida, Styrax grandifolius, and Crataegus marshallii. The patchy short-shrub stratum includes Vaccinium virgatum (= Vaccinium amoenum), Vaccinium arboreum, Vaccinium elliottii, Ilex opaca var. opaca, Chionanthus virginicus, Crataegus marshallii, Frangula caroliniana (= Rhamnus caroliniana), Amelanchier arborea, Callicarpa americana, Ilex ambigua, Viburnum acerifolium, Viburnum dentatum, and Viburnum rufidulum. The sparse herbaceous layer includes Polystichum acrostichoides, Trillium spp., Prenanthes altissima, Spigelia marilandica, Galium circaezans, Desmodium nudiflorum, Uvularia perfoliata, Polygonatum biflorum, Arisaema triphyllum, Viola walteri, Mitchella repens, Tipularia discolor, Lilium michauxii, Smilax herbacea, and Podophyllum peltatum. Magnolia acuminata may be present in a few examples of this type, along the eastern and northern periphery of the region associated with especially moist lower slopes. Rare species that may occur in this community include Prenanthes barbata, Cypripedium kentuckiense, and Triphora trianthophora.
Dynamics: This forest is not a pyrogenic community and experiences very infrequent fires due to its position on generally steep slopes and the lack of available fuel generated by the relatively inflammable deciduous leaf litter. Mesic examples on lower slopes probably burn even less frequently than dry/mesic sites on mid to upper slopes. This association occurs on portions of the landscape where periodic fires were rare to nonexistent, especially mesic steep slopes, and mid to lower slopes along rivers and small streams throughout much of the West Gulf Coastal Plain. The main disturbance vectors in this broad-leaved deciduous forest are windthrow and the active erosion that occurs on the steep slopes. As downstream channelization and gully formation cause streams to erode headward, banks are undercut and erosion is catalyzed on the slopes. This active erosion may contribute to the sparse herbaceous layer. Windstorms, diseases and insects are other disturbances in this uneven-aged forest. Regeneration occurs primarily in canopy gaps (Martin and Smith 1991).
Environmental Description: This forest occurs on acidic soils, typically loamy sands or silt loams including Susquehanna silt loam and Betis and Briley loamy fine sands. Associated geology includes the Sparta, Cockfield, Jackson, Vicksburg, Catahoula, and Fleming formations and Pleistocene High Terraces. Hydrology ranges from dry-mesic to mesic; this community is not subject to flooding. This broad-leaved forest is associated with hilly terrain. The slopes from which this community is known are generally steep, and grade down to riparian forests along streams. It is most common on middle and lower slopes (Martin and Smith 1991).
Geographic Range: This community is known from eastern Texas, western Louisiana, southern Arkansas, and southeastern Oklahoma.
Nations: US
States/Provinces: AR, LA, OK, TX
Plot Analysis Summary:
http://vegbank.org/natureserve/ELEMENT_GLOBAL.2.687981
Confidence Level: Low
Confidence Level Comments: No Data Available
Grank: G3
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.1 Warm Temperate Forest & Woodland Formation | F018 | 1.B.1 |
Division | 1.B.1.Na Southeastern North American Forest & Woodland Division | D006 | 1.B.1.Na |
Macrogroup | 1.B.1.Na.3 American Beech - Southern Magnolia - White Oak Forest Macrogroup | M008 | 1.B.1.Na.3 |
Group | 1.B.1.Na.3.b American Beech - Southern Sugar Maple - White Oak Forest Group | G166 | 1.B.1.Na.3.b |
Alliance | A2059 American Beech - White Oak - Water Oak Coastal Plain Forest Alliance | A2059 | 1.B.1.Na.3.b |
Association | CEGL007208 American Beech - White Oak / American Holly / Southern Ladyfern Forest | CEGL007208 | 1.B.1.Na.3.b |
Concept Lineage: No Data Available
Predecessors: No Data Available
Obsolete Names: No Data Available
Obsolete Parents: No Data Available
Synonomy: < American Beech - White Oak / Mitchella Loamy Moist-Mesic Steep Slopes and Ravines (Turner et al. 1999)
? Beech - Magnolia (69) (USFS 1988)
= Hardwood Slope Forest (Martin and Smith 1991)
= Hardwood Slope Forest (Martin and Smith 1993) [same concept as Martin and Smith (1991)]
< IA8d. Southern Mixed Hardwood Forest (Allard 1990)
< IA8e. Beech - Magnolia Forest (Allard 1990)
< Lower Slope Hardwood Pine Forest (Marks and Harcombe 1981)
? T1B2aI1a. Fagus grandifolia - Ilex opaca (Foti et al. 1994)
? Beech - Magnolia (69) (USFS 1988)
= Hardwood Slope Forest (Martin and Smith 1991)
= Hardwood Slope Forest (Martin and Smith 1993) [same concept as Martin and Smith (1991)]
< IA8d. Southern Mixed Hardwood Forest (Allard 1990)
< IA8e. Beech - Magnolia Forest (Allard 1990)
< Lower Slope Hardwood Pine Forest (Marks and Harcombe 1981)
? T1B2aI1a. Fagus grandifolia - Ilex opaca (Foti et al. 1994)
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