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Forested Wetlands

Primary Question (chapter 20): What are the history, status, and likely future of forested wetlands in the South?

The South has numerous types of forested wetlands, which provide a diverse array of water-quality, flood attenuation, and wildlife habitat benefits. Wetlands of various types have experienced significant structural changes and permanent losses. While the rate of wetland loss is declining, the South has lost more than half of its wetlands between colonial times (1780) and the 1990s.

In the late 1990s, the 10 Southeastern States (the Assessment region minus Virginia, Texas, and Oklahoma) contained approximately 32.6 million acres of forested wetlands (chapter 20). More than half of the region’s wetlands are contained in the Coastal Plain provinces.

Forested wetlands are highly diverse but can be placed into three major categories: riverine, depression, and flatwoods.

Riverine wetlands—They represent the vast majority of forested wetlands in the South. They are located on floodplains and riparian corridors associated with streams and include deepwater swamps and alluvial floodplains that range in size from narrow riparian strips to broad alluvial valleys. The major water sources are overbank flooding and subsurface connections with stream channels. Riverine forested wetlands store water, intercept and cycle nutrients and toxicants, and provide environments for wetland flora and fauna. They may mitigate flood damage, enhance water quality, and support characteristic ecosystems. Because they provide linear connections across landscapes often dominated by other land uses, these types of wetlands also serve as important corridors for the dispersal of wildlife species.

Depression wetlands—They include pocosins, Carolina bays, pond cypress swamps, and mountain fens. These wetlands derive from topographic depressions and receive water from a variety of sources including precipitation, overland flow, and ground water. As with riverine types, benefits are associated with water retention and filtration and provision of wildlife habitat. Most depression wetlands are located low in a watershed, allowing them to play an especially important role in removing sediments, nutrients, and pollutants. Because their vegetative structure is typically very heterogeneous, these areas support highly diverse plant and animal communities. Carolina bays are located throughout the Atlantic Coastal Plain, and cypress domes are located primarily in Florida. Both provide especially important breeding grounds for imperiled amphibians.

Mineral soil flats—They are predominately wet pine flats, shaped by a combination of fire and water regimes. They are commonly found on areas between rivers—called interfluves—on extensive lake bottoms or on large floodplain terraces. The main sources of water are precipitation and slow drainage associated with a landscape of low relief. If subjected to periodic fire, these flats have very few trees. Frequent fire and an uninterrupted hydrologic regime yield a highly diverse and unusual floral assemblage. Their herbaceous species richness is considered to be among the highest in the Western Hemisphere.

Riverine wetland types dominate in the South, representing 91 percent of forested wetland area, compared to approximately 2.5 million acres of mineral soil flats and less than 1 million acres of depression wetlands. We found that (chapter 20):

Drainage and bedding of wetlands can impact soils, hydrologic function, and some species of wildlife. This is an especially important concern for some amphibian species.

An examination of wetland history and status revealed:

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content: David Wear and John Greis
webmaster: John M. Pye

created: 5-OCT-2002
modified: 15-Mar-2007