Portal:Wetlands
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Wetlands Portal
Introduction
A wetland is a land area that is saturated with water, either permanently or seasonally, such that it takes on the characteristics of a distinct ecosystem. The primary factor that distinguishes wetlands from other land forms or water bodies is the characteristic vegetation of aquatic plants, adapted to the unique hydric soil. Wetlands play a number of roles in the environment, principally water purification, flood control, carbon sink and shoreline stability. Wetlands are also considered the most biologically diverse of all ecosystems, serving as home to a wide range of plant and animal life. Wetlands occur naturally on every continent except Antarctica, the largest including the Amazon River basin, the West Siberian Plain, and the Pantanal in South America. The water found in wetlands can be freshwater, brackish, or saltwater. The main wetland types include swamps, marshes, bogs, and fens; and sub-types include mangrove, carr, pocosin, and varzea.
The UN Millennium Ecosystem Assessment determined that environmental degradation is more prominent within wetland systems than any other ecosystem on Earth. International conservation efforts are being used in conjunction with the development of rapid assessment tools to inform people about wetland issues.
Constructed wetlands can be used to treat municipal and industrial wastewater as well as stormwater runoff and they also play a role in water-sensitive urban design.
Selected article
Lake ecosystems are a prime example of lentic ecosystems. Lentic refers to stationary or relatively still water, from the Latin lentus, which means sluggish. Lentic waters range from ponds to lakes to wetlands, and much of this article applies to lentic ecosystems in general. Lentic ecosystems can be compared with lotic ecosystems, which involve flowing terrestrial waters such as rivers and streams. Together, these two fields form the more general study area of freshwater or aquatic ecology.
Lentic systems are diverse, ranging from a small, temporary rainwater pool a few inches deep to Lake Baikal, which has a maximum depth of 1740 m. The general distinction between pools/ponds and lakes is vague, but Brown states that ponds and pools have their entire bottom surfaces exposed to light, while lakes do not. In addition, some lakes become seasonally stratified (discussed in more detail below.) Ponds and pools have two regions: the pelagic open water zone, and the benthic zone, which comprises the bottom and shore regions. Since lakes have deep bottom regions not exposed to light, these systems have an additional zone, the profundal. These three areas can have very different abiotic conditions and, hence, host species that are specifically adapted to live there. (Full article...)
General images
- Image 3The wetlands of Cape May, New Jersey, US, comprise an extensive hydrological network that makes them an ornithologically important location to study the many birds which use the preserve as a place to nest. (from Wetland)
- Image 4Sphagnum moss and sedges can produce floating bog mats along the shores of small lakes. This bog in Duck Lake, Oregon, US, supports populations of English sundew (Drosera anglica). (from Bog)
- Image 5Wetland at the Broadmoor Wildlife Sanctuary in Massachusetts, United States, in February (from Wetland)
- Image 8Marsh Arabs poling a mashoof (from Swamp)
- Image 9Kakerdaja Fen, Estonia (from Fen)
- Image 12Difference between swamp and marsh (from Swamp)
- Image 16Avaste Fen, Estonia. Sedges dominate the landscape, woody shrubs and trees are sparse. (from Fen)
- Image 20Bog-wood and boulders at the Stumpy Knowe near South Auchenmade, Ayrshire, Scotland (from Bog)
- Image 22White water lilies are a typical marsh plant in European areas of deeper water. (from Marsh)
- Image 24Marsh in shallow water on a lakeshore (from Marsh)
- Image 25An expanse of wet Sphagnum bog in Frontenac National Park, Quebec, Canada. Spruce trees can be seen on a forested ridge in the background. (from Bog)
- Image 26A raised bog in Ķemeri National Park, Jūrmala, Latvia, formed approximately 10,000 years ago in the postglacial period and now a tourist attraction. (from Bog)
- Image 27Humid wetland in Pennsylvania before a rain (from Wetland)
- Image 28Sunrise at Viru Bog, Estonia (from Wetland)
- Image 29Small extreme rich fen in southwestern Minnesota. The white flowers, Parnassia glauca, are a fen indicator species in Minnesota. (from Fen)
- Image 32Sugar Fen, Norfolk (from Fen)
- Image 34Marshlands are often noted within wetlands, as seen here in the New Jersey Meadowlands at Lyndhurst, New Jersey, U.S. (from Marsh)
- Image 37Fog rising over the Mukri bog near Mukri, Estonia. The bog has an area of 2,147 hectares (5,310 acres) and has been protected since 1992. (from Wetland)
- Image 39Precipitation accumulates in many bogs, forming bog pools, such as Koitjärve bog in Estonia. (from Bog)
- Image 40Aerial view of prairie potholes (from Marsh)
- Image 41Spaulding Fen, Wisconsin. (from Fen)
- Image 49Marshlands are often noted within wetlands, as seen here at the Jamaica Bay Wildlife Refuge in New York City. (from Wetland)
- Image 50Wetlands contrast the hot, arid landscape around Middle Spring, Fish Springs National Wildlife Refuge, Utah. (from Wetland)
- Image 51Carnivorous plants, such as this Sarracenia purpurea pitcher plant of the eastern seaboard of North America, are often found in bogs. Capturing insects provides nitrogen and phosphorus, which are usually scarce in such conditions. (from Bog)
Law
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Did you know...
... that Spanish moss lowers the growth rate of trees and increases wind resistance?
(Pictured left: Spanish moss.) |
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Categories
Related portals
Organizations
- America's Wetland Foundation
- Birds Korea
- Delta Waterfowl Foundation
- Ducks Unlimited
- Foundation for Ecological Security
- Irish Peatland Conservation Council
- National Wetlands Coalition
- Theodore Roosevelt Conservation Partnership
- Union Sportsmen's Alliance
- Wetlands International
- Wildfowl & Wetlands Trust
Topics
- Acrotelm
- Aquatic ecosystem
- Aquatic plants
- Atchafalaya Basin
- Backswamp
- Bayou
- Beach meadow
- Blackwater river
- Blanket bog
- Bog
- Bog bodies
- Bog butter
- Bog garden
- Bog iron
- Bog snorkelling
- Bog-wood
- Brackish marsh
- Callows
- Carr (landform)
- Cataract bog
- Cienega
- Coniferous swamp
- Converted wetland
- Dambo
- Drainage basin
- Drought refuge
- Estuary
- Everglades
- Fen
- Fen-meadow
- Flark
- Flooded grasslands and savannas
- Flood-meadow
- Floodplain
- Freshwater swamp forest
- Grass valley
- Guelta
- Halosere
- High Fens
- High marsh
- Hamuns
- Hydric soil
- Hydrology
- Hydrosere
- Igapó
- Ings
- Integrated constructed wetland
- Interdunal wetland
- Intertidal wetland
- Kettle (landform)
- Lagoon
- Lake ecosystem
- Limnology
- List of bogs
- List of fen plants
- Low marsh
- Meadowview Biological Research Station
- Marsh
- Marsh gas
- Mere
- Mire
- Misse
- Moorland
- Muck
- Mudflat
- Muskeg
- Myristica swamp
- Oasis
- Ombrotrophic
- Paludification
- Palustrine wetland
- Pantanal
- Peat
- Peat swamp forest
- Pond
- Pothole
- Prairie Pothole Region
- Ramsar site
- Reed bed
- Restoration of the Everglades
- Riparian zone
- River delta
- River ecosystem
- Salt marsh
- Salt marsh dieback
- Salt marsh die-off
- Salt pannes and pools
- Shrub swamp
- Slough (hydrology)
- Sphagnum
- String bog
- Sudd
- Swale
- Swamp
- Tropical peat
- Várzea forest
- Vernal pool
- Water stagnation
- Wetland classification
- Wetland conservation
- Wetland indicator status
- Wetland methane emissions
- Wetlands International
- Wetlands
- Wildfowl & Wetlands Trust
- Will-o'-the-wisp
- Yaéré
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