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CEGL007031 Acer rubrum / Alnus serrulata - Lindera benzoin / Glyceria striata - Impatiens capensis Seep Forest

Type Concept Sentence: No Data Available


Common (Translated Scientific) Name: Red Maple / Hazel Alder - Northern Spicebush / Fowl Mannagrass - Orange Jewelweed Seep Forest

Colloquial Name: Piedmont-Blue Ridge Floodplain Seep Forest

Hierarchy Level:  Association

Type Concept: This community occurs in saturated seepage areas on the edges of active floodplains in the Piedmont and occasionally in the Blue Ridge of North Carolina and possibly South Carolina. It usually occurs in small patches and may be shaded by trees rooted in the adjacent forest or by trees rooted in the wetland. Acer rubrum, Fraxinus pennsylvanica, and Liquidambar styraciflua are most constant, but Betula nigra or other floodplain species are often present and may be abundant. The shrub layer is generally dominated by Alnus serrulata or Lindera benzoin. The herb layer is dense and grassy. Glyceria striata, Cinna arundinacea, and a number of Carex species are dominant. Other abundant herbs include Impatiens capensis, Lycopus virginicus, Boehmeria cylindrica, Sagittaria latifolia, and Polygonum sagittatum.

Diagnostic Characteristics: No Data Available

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: This type was the most distinct of the five types of Piedmont seeps identified in data analysis by Seymour (2011). It may be distinguished by the combination of seep and alluvial species and by the occurrence of both seepage and flooding. Though the defining study was limited to the Piedmont, similar communities have been observed on the Little Tennessee River in the Blue Ridge. In the Piedmont of Virginia, related vegetation is treated as ~Acer rubrum - Fraxinus (pennsylvanica, americana) / Lindera benzoin / Symplocarpus foetidus Swamp Forest (CEGL006406)$$.

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

Physiognomy and Structure: No Data Available

Floristics: These communities have an open to closed tree canopy, which may consist of trees rooted in the wetland or of trees rooted in adjacent communities. Acer rubrum, Fraxinus pennsylvanica, and Liquidambar styraciflua are most constant, but Betula nigra or other floodplain species are often present and may be abundant. The shrub layer ranges from sparse to dense. Alnus serrulata is sometimes strongly dominant. Other examples may have a mix of Lindera benzoin and Alnus or other species. The herbaceous layer is generally dense but not highly diverse. Graminoids usually dominate, including Glyceria striata, Cinna arundinacea, Carex lurida, Carex atlantica ssp. atlantica, Carex atlantica ssp. capillacea (= Carex howei), Carex laevivaginata, Carex crinita, Carex tribuloides, and Carex radiata. Other abundant herbs include Impatiens capensis, Lycopus virginicus, Boehmeria cylindrica, Sagittaria latifolia, and Polygonum sagittatum. Sphagnum spp. or Mnium spp. may be abundant.

Dynamics:  The ongoing wetness created by seepage is the most important ecological influence, but seepage may vary with rainfall. Intermittent flooding and minor sediment deposition may bring in pulses of nutrients and propagules. Flooding and nearby seed sources make these communities highly susceptible to invasion by non-native species. More drastic alterations, such as beaver impoundment or scouring, may alter the community in the long term. Trees likely most often regenerate in small to medium-sized canopy gaps created by wind storms. The saturated soil may make these communities more susceptible to windthrow and keep them dominated by younger canopies than in adjacent communities.

Environmental Description:  This community is found in saturated areas on the edges of active floodplains, fed by seepage from adjacent uplands. It generally occurs on medium to large floodplains in the Piedmont or occasionally the Blue Ridge. These communities have alluvial soils and may be subject to intermittent or occasional floodplain processes, including flooding, sediment deposition, alteration of drainage by nearby erosion or deposition, or impoundment by beavers. They are more constantly influenced by the soil saturation created by groundwater discharge.

Geographic Range: This community occurs in the Piedmont and occasionally in the Blue Ridge of North Carolina and possibly South Carolina and Virginia.

Nations: US

States/Provinces:  NC, SC?




Confidence Level: Low

Confidence Level Comments: No Data Available

Grank: G4

Greasons: No Data Available


Concept Lineage: No Data Available

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: = Floodplain Seeps (Seymour 2011)

Concept Author(s): M.P. Schafale and S.D. Seymour

Author of Description: M.P. Schafale after S.D. Seymour

Acknowledgements: No Data Available

Version Date: 10-04-11

  • Nelson, J. B. 1986. The natural communities of South Carolina: Initial classification and description. South Carolina Wildlife and Marine Resources Department, Division of Wildlife and Freshwater Fisheries, Columbia, SC. 55 pp.
  • Schafale, M. P. 2012. Classification of the natural communities of North Carolina, 4th Approximation. North Carolina Department of Environment, Health, and Natural Resources, Division of Parks and Recreation, Natural Heritage Program, Raleigh.
  • Seymour, S. D. 2011 Vegetation of non-alluvial wetlands of the southeastern Piedmont. M.S. thesis, University of North Carolina, Chapel Hill.
  • Southeastern Ecology Working Group of NatureServe. No date. International Ecological Classification Standard: International Vegetation Classification. Terrestrial Vegetation. NatureServe, Durham, NC.