PIEDMONT LEVEE FOREST (TYPIC SUBTYPE) Concept: Piedmont Levee Forests are forest communities of natural levee deposits or river front riparian zones on large Piedmont floodplains. The Typic Subtype encompasses the common examples where characteristic levee species such as Platanus occidentalis, Betula nigra, Celtis laevigata, and Acer negundo dominate in combination with widespread species such as Liquidambar styraciflua, Liriodendron tulipifera, and Acer rubrum. Fagus grandifolia is scarce or absent. Distinguishing Features: The Piedmont Levee Forest community is distinguished from other communities of large Piedmont floodplains, as well as uplands, by significant presence of the characteristic levee species: Platanus occidentalis, Betula nigra, Acer negundo, and Celtis laevigata in natural condition. Fraxinus pennsylvanica too distinguishes it from communities other than Piedmont Swamp Forest. It is distinguished from Piedmont Alluvial Forest by occurring on larger floodplains — those with differentiated levee, bottomland, and terrace zones large enough to support distinct communities. The distinguishing characteristic is the size of the floodplain, not the river. Where large rivers flow through confined areas without extensive floodplain development, the narrow floodplains generally support Piedmont Alluvial Forest, with a mix of levee, bottomland, and upland species. However, occasionally they will more resemble a Piedmont Levee Forest. While Piedmont Levee Forest usually occurs along large rivers, it also occurs in the wide floodplains that develop along medium size creeks in Triassic basins. Piedmont Levee Forests are distinguished from Montane Alluvial Forests by the absence of characteristic montane species such as Tsuga canadensis, Pinus strobus, and various herb species shared with Rich Cove Forest. The Typic Subtype is distinguished by dominance by typical floodplain species, with little or no presence of Fagus grandifolia and limited component of other upland species. Synonyms: Fraxinus pennsylvanica – Platanus occidentalis – Celtis laevigata / Chasmanthium latifolium Piedmont River Levee Forest (CEGL007013). Ecological Systems: Southern Piedmont Large Floodplain Forest (CES202.324). Sites: Piedmont Levee Forests occur on natural levees, stable forested point bar deposits, or on the river front edge of flatter terraces. They occur on broad floodplains, usually along larger rivers. They may also occur on creeks as small as 3rd order in Triassic basins, where broad floodplains form more readily. Even on larger rivers, Piedmont Levee Forests require a substantial floodplain and are generally absent where floodplain width is limited. Soils: Soils are coarse or medium-textured, formed in recent alluvial deposits with little or no horizon development. Most examples are mapped as Congaree (Typic Udifluvent), Chewacla (Fluvaquentic Dystrudept), or Wehadkee (Fluvaquentic Endoaquept). Soils are among the most fertile in the Piedmont, thanks to ongoing nutrient input. Hydrology: Piedmont Levee Forests are intermittently flooded for short periods. The flood flow can have substantial current. Vegetation: Piedmont Levee Forests are naturally closed forests punctuated by canopy gaps. The forest is a varying mix of a large pool of possible species. Frequent species in Matthews, et al. (2011) and site descriptions include Fraxinus pennsylvanica, Platanus occidentalis, Betula nigra, Celtis laevigata, Acer negundo, Liquidambar styraciflua, Liriodendron tulipifera, Ulmus americana, Ulmus alata, Juglans nigra, Acer floridanum, and Acer rubrum. Less frequent trees include Quercus phellos, Carya cordiformis, Carya ovata, Carya carolinae-septentrionalis, Quercus michauxii, Quercus nigra, Quercus pagoda, and a few Quercus alba, Quercus rubra, or Fagus grandifolia. The understory is frequently dominated by Carpinus caroliniana, Acer negundo, or Asimina triloba. Other species, such as Ilex opaca, Cornus florida, or Nyssa sylvatica, may also occur. The shrub layer is general moderate to fairly dense. Dominant species are most often Ilex decidua, Lindera benzoin, Arundinaria tecta, or currently, exotic species such as Ligustrum sinense. Other shrubs include Aesculus sylvatica, Viburnum prunifolium, Alnus serrulata, or the exotic Rosa multiflora. Vines are often extensive and fairly diverse. Highly constant species include Toxicodendron radicans, Smilax rotundifolia, Muscadinia rotundifolia, Parthenocissus quinquefolia, Bignonia capreolata, and the exotic Lonicera japonica, less constant Campsis radicans, Thyrsanthella difforme, and Vitis sp. The herb layer is generally dense, sometimes lush. Chasmanthium latifolium or Elymus virginicus, or exotic species such as Microstegium vimineum or Glechoma hederacea may dominate, but often it is a diverse mix with no strong dominant. The most constant additional species include Boehmeria cylindrica, Arisaema triphyllum, several Carex species (e.g., radiata, amphibola), Festuca subverticillata, Persicaria virginiana, Glyceria striata, Galium aparine, and Viola spp. Fairly frequent species include Polystichum acrostichoides, Persicaria spp., Laportea canadensis, Carex intumescens, Carex typhina, Sanicula canadensis, Geum canadense, Pilea pumila, Verbesina alternifolia, Verbesina occidentalis, Commelina virginica, Dichanthelium commutation, Leersia virginica, Lycopus virginicus, Impatiens capensis, Juncus coriaceus, and Solidago sp. Other herbs that are lower constancy in plot data but appear characteristic include Elymus hystrix, Corydalis flavula, Osmorhiza longistylis, Asarum canadense, Melica mutica, and Arisaema dracontium. Range and Abundance: Ranked G3G4. This community occurs throughout the Piedmont except in the foothills area. Recognizable examples are abundant on large rivers and are often present when no other floodplain communities remain. A strip is often left when the rest of a floodplain is cleared or clearcut, and higher levees may remain forested when lower areas are drowned by impoundments. However, examples that are at full natural width, not subject to extreme edge effects from both sides, and not dominated by exotic plants in one or more strata are rarer. Examples without hydrology modified by upstream dams or urbanization are more rare still. The equivalent NVC association ranges from Virginia to Georgia. Associations and Patterns: Piedmont Levee Forests occur naturally as large patch communities, forming continuous, though fairly narrow, bands that would add up to substantial acreage. Many examples now exist as small patches. Piedmont Levee Forest grades into Piedmont Swamp Forest or Piedmont Bottomland Forest away from the channel. It usually is bordered by the river channel, but Sand and Mud Bar or Rocky Bar and Shore communities may border it. Variation: Plot data analysis by Matthews, et al. (2011) recognized two kinds of levee forests, which are treated as variants. However, they noted substantial overlap in settings and soil characteristics. The author, too, has observed the nominal plant species in different combinations. These variants need further investigation into how distinct they are. 1. Sugarberry-Elm Variant, which they named Ulmus americana–Celtis laevigata/Lindera benzoin/Osmorhiza longistylis tends to occur farther downstream, on larger floodplains, and to be more fertile. 2. Ash-Sycamore Variant, which they named Fraxinus pennsylvanica–Platanus occidentalis/Acer negundo/Chasmanthium latifolium tends to occur farther upstream, farther inland, tends toward smaller floodplains, and though fertile, is somewhat less so. The composition suggests an earlier stage of succession, but given its occurrence in different settings, as well as the avoidance of obviously successional vegetation in CVS sampling, it is more likely a result of different flooding dynamics. Dynamics: General dynamics of Piedmont Levee Forests are similar to Piedmont and Mountain Floodplains in general. The current during floods is stronger on the levees than in most other parts of the floodplain. Vegetation may be battered by floating debris and soil may be locally scoured, though it is rare for large plants to be killed by this. Some tree mortality occurs through undercutting along the riverbank. Conversely, new deposition of bars can create new sites for forest development; however, these processes appear much slower than in the Coastal Plain, despite the stronger currents and greater potential for sediment movement. Natural levees form because sediment deposition is concentrated on the riverbank. The coarsest material falls out there; sand deposits are common, though a layer of silt and clay is also left at the end of floods. The periodic input of nutrients in flood-deposited sediment makes levee sites very fertile, perhaps the most fertile sites in the Piedmont, and plant growth is rapid in these communities. The levees may have been the most affected by the massive influx of sediment during the early decades of European agriculture and by ongoing changed conditions. Rates of erosion in uplands remain higher than natural. The loss of forest cover and the increase in bare ground and impervious surfaces has led to faster runoff, while large dams have altered flood regimes and have removed sediment from some reaches. Piedmont Levee Forests are among the most susceptible communities to invasion by exotic plants, due to a combination of high fertility, higher light levels along the bank, creation of bare ground patches by flood scouring and wrack movement, and dispersal of seeds by floodwaters.