| Part I: Background information on wetlands |
Wetlands
According to the EPA..
"Wetlands are areas where water covers the soil, or is present either at or near the surface of the soil all year or for varying periods of time during the year, including during the growing season. Water saturation largely determines how the soil develops and the types of plant and animal communitites living in and on the soil. Wetlands may support both aquatic and terrestrial species. The prolonged presence of water creates conditions that favor the growth of specially adapted plants and promote the development of characteristic wetlands soils."
* Marshes include: tidal and nontidal (covered later)
* Wet Meadows inlude : Prairie Potholes + Vernal Pools + Playa Lakes
* Swamps include: Forested Swamps + Bottomland Hardwoods + Shrub Swamps +Mangrove Swamps ( covered later)
* Bogs include: Northern bogs + Pocosins ( southern bogs) + Fens
Swamps
A swamp is any wetland dominated by woody plants. There are
many different kinds of swamps, ranging from the forested red maple, (Acer rubrum),
swamps of the Northeast, to the extensive bottomland hardwood forests found
along the sluggish rivers of the Southeast.
Swamps are characterized by saturated soils during the growing season, and standing water during certain times of the year. The highly organic soils of swamps form a thick, black, nutrient-rich environment for the growth of water-tolerant trees such as cypress (Taxodium spp.), Atlantic white cedar (Chamaecyparis thyoides), and tupelo (Nyssa aquatica).Some swamps are dominated by shrubs, such as buttonbush or smooth alder.
Birds, fish, and invertebrates such as freshwater shrimp, crayfish,
and clams require the habitats provided by swamps. Many rare species,
such as the endangered American crocodile depend on these ecosystems as well.
Skunk Cabbage (Symplocarpus foetidus) sprouts very early in the spring, melting
the surrounding snow. The insects that pollinate it are attracted by its odor,
which resembles decaying flesh.
Origin and Development
Swamps develop in depressions where there is poor drainage and/or the
water table is high. Despite the water trapped in these areas, they
are colonized by trees. These forested wetlands develop in still or slowing
flowing water around lake margins, along floodplains, and by oxbow lakes.
Poorly drained depressions and areas subject to periodic flooding have mucky
soils that are too wet for surrounding forest species but are ideal for swamp
plants.
Swamps may evolve from sedge and cattail marshes as water levels decrease due to organic matter accumulation, sedimentation or lowering of the water table. As water levels decrease, red maples and other swamp species become established and as they grow, they shade out light demanding marsh plants. Marsh animals such as ducks and muskrats leave the area and are replaced by swamp species.
Swamps may develop on the surface of old fens and bogs (peatlands), after terrestrialization
is complete. In fact conifer swamps are often mistaken for bogs. As a bog develops,
the open water area may eventually be covered with a vegetative mat and trees
can become well established. However, the presence of moss and wet,
spongy ground distinguishes a bog from a swamp. A conifer swamp is
established with the same trees as a bog, but there is no moss and the area
is flooded for a part of the year with water from rivers, lakes, spring runoff
or groundwater.
Vegetation and Wildlife
The vegetation in swamps is predominately dense coniferous or deciduous forest
or tall shrub thickets. The trees which inhabit a swamp are dependent upon climatic
conditions.
Northern boreal swamps are usually dominated by white and
black spruce but more nutrient-rich sites have cedars.
As one progresses south, red or silver maple, ash and yellow
birch become more common in swamps. . Ferns, blueberries, touch-me-nots, orchids,
and skunk cabbage are common swamp plants.
Swamps provide habitat for a wide variety of wildlife and in many parts, swamps
are the only remaining natural cover for larger wildlife. Common swamp animals
include wood frogs, salamanders, and both wood and black ducks.
Cypress Swamps
Cypress swamps are found in the southern United States. They are named
for the bald cypress tree. Bald cypress trees are deciduous trees with needle-like
leaves. They have very wide bases and "knees" that grow from
their roots and stick up out of the water. Bald cypress trees can grow
to 100 to 120 feet tall. Fire plays an important role in the establishment
of bald cypress swamps. Cypress trees grow very quickly after a fire and
reestablish themselves before other trees have a chance to grow! Many
of the bald cypress trees in cypress swamps in the U.S. were cut down in the
late 1800's and the early 1900's. The wood from the bald cypress is resistant
to rot and was a popular wood for building. Other trees and shrubs like
pond cypress , blackgum, red maple, wax myrtle, and buttonwood can also be found
in cypress swamps. Animals like white-tailed deer, minks, raccoons,
anhingas, pileated woodpeckers, purplegallinules, egrets, herons, alligators,
frogs, turtles, and snakes are often found in cypress swamps.
From Lake to Swamp
Swamps start out as lakes, ponds or other shallow bodies of water. Over
time, trees and shrubs begin to fill in the land. Plants die and decay
and the level of the water gets lower and lower. Eventually, the original body
of water becomes a swamp.
Okefenokee Swamp
The Okefenokee Swamp is located in southeastern Georgia and northern Florida.
It is about 25 miles wide and 40 miles long. Not all of the Okefenokee
is a swamp, part of it is a bog. In fact, Okefenokee is an Indian word
that means "Land of the Trembling Earth." Parts of the swamp
are so boggy that you can shake the trees by stomping on the ground! Trees
in the Okefenokee swamp include giant tupelo and bald cypress. Mammals
like the raccoon, black bear, white-tailed deer, bobcats, redfox, and river
otter make the swamp their home. Reptiles in the swamp include the eastern diamondback
rattlesnake, cottonmouth, eastern coral snake, copper head, alligator,
and snapping turtle. Birds like the barred owl, anhinga, great egret,
great blue heron, and sandhill crane are also found in the swamp. Plants like
the pitcher plant, water lily, and spanish moss that grow in the swamp can survive
in the nutrient poor soil and acidic soil of the Okefenokee swamp.
Functions &Values
Swamps serve vital roles in flood protection and nutrient removal. Floodplain
forests are especially high in productivity and species diversity because of
the rich deposits of alluvial soil from floods. Many upland creatures depend
on the abundance of food found in the lowland swamps, and valuable timber can
be sustainably harvested to provide building materials for people.
In very dry years they may represent the only shallow water for miles and their presence is critical to the survival of wetland-dependent species like wood ducks (Aix sponsa), river otters (Lutra canadensis), and cottonmouth snakes (Agkistrodon piscivorus).
Status
Due to the nutrient-rich soils present in swamps, many of these fertile woodlands
have been drained and cleared for agriculture and other development. Over
70 percent of the Nation's floodplain forested swamps have been lost.
Historically, swamps have been portrayed as frightening no-man's-lands. This
perception led to the vast devastation of immense tracts of swampland over the
past 200 years, such as the destruction of more than half of the legendary Great
Dismal Swamp of southeastern Virginia.
Shrub swamps
Shrub swamps, are similar to forested swamps, except that shrubby vegetation
such as buttonbush, willow, dogwood (Cornus sp.) , and swamp rose (Rosa palustris)
predominates. In fact, forested and shrub swamps are often found adjacent to
one another. The soil is often water logged for much of the year, and covered
at times by as much as a few feet of water because this type of swamp is found
along slow moving streams and in floodplains. Mangrove swamps are a type of
shrub swamp dominated by mangroves that covers vast expanses of southern Florida.
Bogs
Sphagnum creates bogs by holding water and creating acidic conditions.
Sphagnum itself may be up to 70 percent water.
Bogs are one of North America's most distinctive kinds of wetlands. They are
characterized by spongy peat deposits, acidic waters, and a floor covered by
a thick carpet of sphagnum moss.
Bogs receive all or most of their water from precipitation rather than from
runoff, groundwater or streams. As a result, bogs are low in the nutrients needed
for plant growth, a condition that is enhanced by acid forming peat mosses.
There are two primary ways that a bog can develop:
--> bogs can form as sphagnum moss grows over a lake or pond and slowly fills
it (terrestrialization), or
--> bogs can form as sphagnum moss blankets dry land and prevents water from
leaving the surface (paludification).
Over time, many feet of acidic peat deposits build up in bogs of either origin. The unique and demanding physical and chemical characteristics of bogs result in the presence of plant and animal communities that demonstrate many special adaptations to low nutrient levels, waterlogged conditions, and acidic waters, such as carnivorous plants.
Functions and Values
Bogs serve an important ecological function in preventing downstream flooding
by absorbing precipitation.
Bogs support some of the most interesting plants in the United States (like
the carnivorous sundew), and provide habitat to animals threatened by human
encroachment.
Status
Bogs are mostly found in the glaciated northeast and Great Lakes regions (northern
bogs), as well as in the southeast (pocosins). Their acreage declined historically,
as they were drained to be used as cropland, and mined for their peat which
was used as a fuel and a soil conditioner. Recently, bogs have been recognized
for their role in regulating the global climate by storing large amounts of
carbon in peat deposits. Bogs are unique communities that can be destroyed in
a matter of days, but require hundreds, if not thousands, of years to form naturally.
Fens
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Fens, like bogs, are peatlands, but because
they are fed by groundwater they are not so acidic as bogs. Fens differ from bogs because they are less acidic and have higher nutrient levels. They are therefore able to support a much more diverse plant and animal community. These systems are often covered by grasses, sedges, rushes, and wildflowers.
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| Over time, peat may build up and separate the fen from its
groundwater supply. When this happens, the fen receives fewer nutrients
and may become a bog. Like bogs, fens are mostly a northern hemisphere phenomenon -- occurring in the northeastern United States, the Great Lakes region, the Rocky Mountains, and much of Canada -- and are generally associated with low temperatures and short growing seasons, where ample precipitation and high humidity cause excessive moisture to accumulate. |
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Functions & Values
Fens, like bogs, provide important benefits in a watershed, including preventing
or reducing the risk of floods, improving water quality, and providing habitat
for unique plant and animal communities.
Status
Like most peatlands, fens experienced a decline in acreage at a rate of about
eight percent from 1950 to 1970, mostly from mining and draining for cropland,
fuel, and fertilizer.
Fens may be dominated by woody or herbaceous vegetation. Trees often invade
herbaceous fens, making true. that much more rare. It is important to recognize
that while mining and draining these ecosystems provide resources for people,
up to 10,000 years are required to form a fen naturally.
| Part II: Examples of Swamps & Bogs |
1. Visit the Okeefenokee Swamp ( online link here.. be forewarned this is a multipage site! )
2. Visit a northern bog ( class project)
3. Visit the Everglades ( video if time)