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Wetland types found in the US

 

Time lapsed animation of basin from 1956 to 1993.

Time lapsed animation of basin from 1956 to 1993.

 

Inland fresh areas

 

Wetland functions

By absorbing the force of strong winds and tides, wetlands protect terrestrial areas adjoining them from storms, floods, and tidal damage. Wetlands remove nutrients from surface and ground water by filtering and by converting nutrients to unavailable forms. Denitrification is arguably the most important of these reactions because humans have increased nitrate worldwide by applying fertizers. Increased nitrate availability can cause eutrophication, but denitrification converts biolgically available nitrogen back into nitrogen gas, which is biologically unavailable except to nitrogen fixing bacteria. Denitrification can be detected in many soils, but denitrification is fastest in wetlands soils (for an example, see Ullah and Faulkner 2006). Many wetlands also provide habitat for resident and migratory fish and wildlife.

Intertidal wetlands provide an excellent example of invasion, modification and succession. The invasion and succession process is establishment of seagrasses. These help stabilize sediment and increase sediment capture rates. The trapped sediment gradually develops into mud flats. Mud flat organisms become established encouraging other life forms changing the organic composition of the soils.

The mangroves establish themselves in the shallower water upslope from the mudflats. Mangroves further stabilize sediment and over time increase the soil level. This results in less tidal movement and the development of salt marshes. (succession) The salty nature of the soil means it can only be tolerated by special types of grasses e.g. saltbush, rush and sedge. There is also changing species diversity in each succession.

In the salt marshes there is greater species diversity, nutrient recycling, and niche specialisation making it one of the most productive ecosystems on Earth.

Small wetland in Marshall County, Indiana.

Small wetland in Marshall County, Indiana.

 

Adjustments to natural stress

In intertidal wetlands the majority of natural stress comes from salinity and tidal movements. The intertidal wetlands must be able to survive extreme conditions of mainly salt water at high tide, fresh water at low tide and times of flood and brackish water at other times. The saline water is a very difficult condition for plants to survive in. The grey mangrove accomplishes this by excluding salt in the root system, salt glands in the leaf, and waxy leaves to minimize water loss. However it is vulnerable to changes in salinity levels.

Changes to tidal movements through increased run-off or altered drainage can cause the roots of mangroves to be inundated for longer than normal periods affecting their pneumatophones. It can also be pushed past its threshold level if water quality is changed. Thus even healthy ecosystems are vulnerable to change.

Some species such as oysters and molluscs have been used as indicator species, with any decline in their numbers indicating the ecosystem is under stress. A change in nutrient levels may also affect primary productivity and thus bring about change.

Wetlands are often filled in to be used by humans for everything from agriculture to parking lots, in part because the economic value of wetlands has only been recognized recently: the shrimp and fish that breed in salt water marshes are generally harvested in deeper water, for example.

Humans can maximize the area of healthy, functioning intertidal wetlands by minimising their impacts and by developing management strategies that protect, and where possible rehabilitate those ecosystems at risk.

 

Protecting or rehabilitating wetlands

A temperate wetland in Britain, with shallow open water and reedbeds.

A temperate wetland in Britain, with shallow open water and reedbeds.

Historically, humans have made large-scale efforts to drain wetlands for development or flood them for use as recreational lakes. Since the 1970s, more focus has been put on preserving wetlands for their natural function—sometimes also at great expense. One example is the project by the U.S. Army Corps of Engineers to control flooding and enhance development by taming the Everglades, a project which has now been reversed to restore much of the wetlands as a natural habitat and method of flood control.

  1. Exclusion—Those responsible for the management of wetland areas often facilitate public access to a small, designated area while restricting access to other areas. Provision of defined boardwalks and walkways is a management strategy used to restrict access to vulnerable areas, as is the issuing of permits whilst visiting.
  2. Education—In the past, wetlands were regarded as wastelands. Education campaigns have helped to change public perceptions and foster public support for the wetlands. Due to their location in the catchment area, education programs need to teach about total catchment management programs. Educational programs include guided tours for the general public, school visits, media liaison, and information centers.

 

Politics and Regulation of Wetlands Protection

 

In the USA

In the United States, some wetlands are regulated by the federal government under the Clean Water Act. Determining the boundary between regulated wetlands and non-regulated lands therefore can be contentious. Deciding where that boundary lies is as easy as determining the boundary between rock-n-roll music and country music, or between legal highway speeds and illegal highway speeds. In reality, there is no natural boundary between the classes that humans define on these gradients (wetland/upland, rock-n-roll/country, speeding/not speeding), and this issue is highlighted by the US. Fish and Wildlife Service’s definition from Classification of Wetlands and Deepwater Habitats of the United States, which defines wetlands as “lands transitional between terrestrial and aquatic systems.” Regulations to protect water quality and highway safety require that we create arbitrary boundaries within those gradients, but these boundaries are scientifically definable, and consist of areas where three criterion of the presence of hydric soils, the presence of wetland vegetation, and the presence of appropriate hydrology. Such regulations must be predictable, reproducible, and enforced. Otherwise, we will sacrifice clean water for development in the case of wetlands regulation (or vice versa), or sacrifice safe travel for quick travel (or vice versa) in the case of speed limits. Determining which wetlands are regulated under section 404 of the clean water act or section 10 of the rivers and harbors act is termed “jurisdictional determination.” Determining the boundary of wetland, whether jurisdictional under sections 404 or 10, or not jurisdictional but still meeting the technical definition of a wetland, that is having the soils, vegetation and hydrology criterion met is called a "wetland delineation," and generally is performed by college graduates with science or engineering degrees working for engineering firms or environmental consulting firms who are familiar with the 1987 U.S. Army Corps of Engineers Wetland delineation manual. Defining a boundary depends upon soil and vegetation characteristics; it is easier to do where the slope of the land is steeper. Deciding if a wetland is a regulated wetland depends on classifying the water in it as “water of the United States” or not. Classifying water as “of the U.S.” or “not of the U.S.” for purposes of enforcing the Clean Water Act suggests a natural boundary that probably does not exist in nature, and one that was not created regarding air for purposes of enforcing the Clean Air Act.

Wetlands are the focus of the US National Wetlands Coalition, which in turn has become the focus of some controversy over "false fronts," a form of political camouflage.

 

Notes

  1. ^ Definition from Corps of Engineers Wetlands Delineation Manual by Environmental Laboratory U.S. Army Corps of Engineers Waterways Experiment Station 3909 Halls Ferry Road Vicksburg, MS 39180-6199

Ullah, S; Faulkner, SP. 2006. Denitrification potential of different land-use types in an agricultural watershed, lower Mississippi valley. ECOLOGICAL ENGINEERING 28 (2): 131-140.

 

 

 

Wikipedia

http://en.wikipedia.org/w/index.php?title=Wetland&action=history

http://www.gnu.org/copyleft/fdl.html