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Wetland

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For other uses, see Wetland (disambiguation).
Upland vs. wetland vs. lacustrine zones
Freshwater swamp forest in Bangladesh
Peat bogs are freshwater wetlands that develop in areas with standing water and low soil fertility.
Mount Polley wetlands in British Columbia, Canada
Wetlands come in different sizes and types. From top left: Upland vs. wetland vs. lacustrine zones; freshwater swamp forest in Bangladesh; peat bogs are freshwater wetlands that develop in areas with standing water and low soil fertility; a freshwater cattail (Typha) marsh that develops with standing water and high soil fertility.

A wetland is a distinct semi-aquatic ecosystem whose groundcovers are flooded or saturated in water, either permanently, for years or decades, or only seasonally. Flooding results in oxygen-poor (anoxic) processes taking place, especially in the soils.[1] Wetlands form a transitional zone between waterbodies and dry lands, and are different from other terrestrial or aquatic ecosystems due to their vegetation's roots having adapted to oxygen-poor waterlogged soils.[2] They are considered among the most biologically diverse of all ecosystems, serving as habitats to a wide range of aquatic and semi-aquatic plants and animals, with often improved water quality due to plant removal of excess nutrients such as nitrates and phosphorus.

Wetlands exist on every continent, except Antarctica.[3] The water in wetlands is either freshwater, brackish or saltwater.[2] The main types of wetland are defined based on the dominant plants and the source of the water. For example, marshes are wetlands dominated by emergent herbaceous vegetation such as reeds, cattails and sedges. Swamps are dominated by woody vegetation such as trees and shrubs (although reed swamps in Europe are dominated by reeds, not trees). Mangrove forest are wetlands with mangroves, halophytic woody plants that have evolved to tolerate salty water.

Examples of wetlands classified by the sources of water include tidal wetlands, where the water source is ocean tides); estuaries, water source is mixed tidal and river waters; floodplains, water source is excess water from overflowed rivers or lakes; and bogs and vernal ponds, water source is rainfall or meltwater.[1][4] The world's largest wetlands include the Amazon River basin, the West Siberian Plain,[5] the Pantanal in South America,[6] and the Sundarbans in the Ganges-Brahmaputra delta.[7]

Wetlands contribute many ecosystem services that benefit people. These include for example water purification, stabilization of shorelines, storm protection and flood control. In addition, wetlands also process and condense carbon (in processes called carbon fixation and sequestration), and other nutrients and water pollutants. Wetlands can act as a sink or a source of carbon, depending on the specific wetland. If they function as a carbon sink, they can help with climate change mitigation. However, wetlands can also be a significant source of methane emissions due to anaerobic decomposition of soaked detritus, and some are also emitters of nitrous oxide.[8][9]

Humans are disturbing and damaging wetlands in many ways, including oil and gas extraction, building infrastructure, overgrazing of livestock, overfishing, alteration of wetlands including dredging and draining, nutrient pollution, and water pollution.[10][11] Wetlands are more threatened by environmental degradation than any other ecosystem on Earth, according to the Millennium Ecosystem Assessment from 2005.[12] Methods exist for assessing wetland ecological health. These methods have contributed to wetland conservation by raising public awareness of the functions that wetlands can provide.[13] Since 1971, work under an international treaty seeks to identify and protect "wetlands of international importance."

Definitions and terminology

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Marshlands are often noted within wetlands, as seen here at the Jamaica Bay Wildlife Refuge in New York City.

Technical definitions

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A simplified definition of wetland is "an area of land that is usually saturated with water".[14] More precisely, 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".[15] A patch of land that develops pools of water after a rain storm would not necessarily be considered a "wetland", even though the land is wet. Wetlands have unique characteristics: they are generally distinguished from other water bodies or landforms based on their water level and on the types of plants that live within them. Specifically, wetlands are characterized as having a water table that stands at or near the land surface for a long enough period each year to support aquatic plants.[16][17]

A more concise definition is a community composed of hydric soil and hydrophytes.[1]

Wetlands have also been described as ecotones, providing a transition between dry land and water bodies.[18] Wetlands exist "...at the interface between truly terrestrial ecosystems and aquatic systems, making them inherently different from each other, yet highly dependent on both."[11]

In environmental decision-making, there are subsets of definitions that are agreed upon to make regulatory and policy decisions.

Under the Ramsar international wetland conservation treaty, wetlands are defined as follows:[19]

  • Article 1.1: "...wetlands are areas of marsh, fen, peatland or water, whether natural or artificial, permanent or temporary, with water that is static or flowing, fresh, brackish or salt, including areas of marine water the depth of which at low tide does not exceed six meters."
  • Article 2.1: "[Wetlands] may incorporate riparian and coastal zones adjacent to the wetlands, and islands or bodies of marine water deeper than six meters at low tide lying within the wetlands."

An ecological definition of a wetland is "an ecosystem that arises when inundation by water produces soils dominated by anaerobic and aerobic processes, which, in turn, forces the biota, particularly rooted plants, to adapt to flooding".[1]

Sometimes a precise legal definition of a wetland is required. The definition used for regulation by the United States government is: 'The term "wetlands" means those areas that are inundated or saturated by surface or ground water at a frequency and duration to support, and that under normal circumstances do support, a prevalence of vegetation typically adapted for life in saturated soil conditions. Wetlands generally included swamps, marshes, bogs, and similar areas.'[20]

For each of these definitions and others, regardless of the purpose, hydrology is emphasized (shallow waters, water-logged soils). The soil characteristics and the plants and animals controlled by the wetland hydrology are often additional components of the definitions.[21]

Types

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Sunrise at Viru Bog, Estonia
Main article: Classification of wetlands

Wetlands can be tidal (inundated by tides) or non-tidal.[15] The water in wetlands is either freshwater, brackish, saline, or alkaline.[2] There are four main kinds of wetlands – marsh, swamp, bog, and fen (bogs and fens being types of peatlands or mires). Some experts also recognize wet meadows and aquatic ecosystems as additional wetland types.[1] Sub-types include mangrove forests, carrs, pocosins, floodplains,[1] peatlands, vernal pools, sinks, and many others.[22]

The following three groups are used within Australia to classify wetland by type: Marine and coastal zone wetlands, inland wetlands and human-made wetlands.[23] In the US, the best known classifications are the Cowardin classification system[24] and the hydrogeomorphic (HGM) classification system. The Cowardin system includes five main types of wetlands: marine (ocean-associated), estuarine (mixed ocean- and river-associated), riverine (within river channels), lacustrine (lake-associated) and palustrine (inland nontidal habitats).

Peatlands

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Peatlands are a unique kind of wetland where lush plant growth and slow decay of dead plants (under anoxic conditions) results in organic peat accumulating; bogs, fens, and mires are different names for peatlands.

Wetland names

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Variations of names for wetland systems:

Some wetlands have localized names unique to a region such as the prairie potholes of North America's northern plain, pocosins, Carolina bays and baygalls[25][26] of the Southeastern US, mallines of Argentina, Mediterranean seasonal ponds of Europe and California, turloughs of Ireland, billabongs of Australia, among many others.

Locations

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By temperature zone

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Wetlands contrast the hot, arid landscape around Middle Spring, Fish Springs National Wildlife Refuge, Utah.

Wetlands are found throughout the world in different climates.[15] Temperatures vary greatly depending on the location of the wetland. Many of the world's wetlands are in the temperate zones, midway between the North or South Poles and the equator. In these zones, summers are warm and winters are cold, but temperatures are not extreme. In subtropical zone wetlands, such as along the Gulf of Mexico, average temperatures might be 11 °C (52 °F). Wetlands in the tropics are subjected to much higher temperatures for a large portion of the year. Temperatures for wetlands on the Arabian Peninsula can exceed 50 °C (122 °F) and these habitats would therefore be subject to rapid evaporation. In northeastern Siberia, which has a polar climate, wetland temperatures can be as low as −50 °C (−58 °F). Peatlands in arctic and subarctic regions insulate the permafrost, thus delaying or preventing its thawing during summer, as well as inducing its formation.[27]

By precipitation amount

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The amount of precipitation a wetland receives varies widely according to its area. Wetlands in Wales, Scotland, and western Ireland typically receive about 1,500 mm (59 in) per year.[citation needed] In some places in Southeast Asia, where heavy rains occur, they can receive up to 10,000 mm (390 in).[citation needed] In some drier regions, wetlands exist where as little as 180 mm (7.1 in) precipitation occurs each year.[citation needed]

Temporal variation:[28]

Surface flow may occur in some segments, with subsurface flow in other segments.

Processes

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Wetlands vary widely due to local and regional differences in topography, hydrology, vegetation, and other factors, including human involvement. Other important factors include fertility, natural disturbance, competition, herbivory, burial and salinity.[1] When peat accumulates, bogs and fens arise.

Hydrology

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The wetlands of Cape May, New Jersey, in the United States 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.
A wetland in the Chesapeake Bay drainage basin in Mallows Bay Park in Charles County, Maryland, in the United States.

The most important factor producing wetlands is hydrology, or flooding. The duration of flooding or prolonged soil saturation by groundwater determines whether the resulting wetland has aquatic, marsh or swamp vegetation. Other important factors include soil fertility, natural disturbance, competition, herbivory, burial, and salinity.[1] When peat from dead plants accumulates, bogs and fens develop.

Wetland hydrology is associated with the spatial and temporal dispersion, flow, and physio-chemical attributes of surface and ground waters. Sources of hydrological flows into wetlands are predominantly precipitation, surface water (saltwater or freshwater), and groundwater. Water flows out of wetlands by evapotranspiration, surface flows and tides, and subsurface water outflow. Hydrodynamics (the movement of water through and from a wetland) affects hydro-periods (temporal fluctuations in water levels) by controlling the water balance and water storage within a wetland.[29]

Landscape characteristics control wetland hydrology and water chemistry. The O2 and CO2 concentrations of water depend upon temperature, atmospheric pressure and mixing with the air (from winds or water flows). Water chemistry within wetlands is determined by the pH, salinity, nutrients, conductivity, soil composition, hardness, and the sources of water. Water chemistry varies across landscapes and climatic regions. Wetlands are generally minerotrophic (waters contain dissolved materials from soils) with the exception of ombrotrophic bogs that are fed only by water from precipitation.

Because bogs receive most of their water from precipitation and humidity from the atmosphere, their water usually has low mineral ionic composition. In contrast, wetlands fed by groundwater or tides have a higher concentration of dissolved nutrients and minerals.

Fen peatlands receive water both from precipitation and ground water in varying amounts so their water chemistry ranges from acidic with low levels of dissolved minerals to alkaline with high accumulation of calcium and magnesium.[30]

Role of salinity

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Salinity has a strong influence on wetland water chemistry, particularly in coastal wetlands[1][31] and in arid and semiarid regions with large precipitation deficits. Natural salinity is regulated by interactions between ground and surface water, which may be influenced by human activity.[32]

Soil

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Carbon is the major nutrient cycled within wetlands. Most nutrients, such as sulfur, phosphorus, carbon, and nitrogen are found within the soil of wetlands. Anaerobic and aerobic respiration in the soil influences the nutrient cycling of carbon, hydrogen, oxygen, and nitrogen,[33] and the solubility of phosphorus[34] thus contributing to the chemical variations in its water. Wetlands with low pH and saline conductivity may reflect the presence of acid sulfates[35] and wetlands with average salinity levels can be heavily influenced by calcium or magnesium. Biogeochemical processes in wetlands are determined by soils with low redox potential.[36]

Biology

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The life forms of a wetland system includes its plants (flora) and animals (fauna) and microbes (bacteria, fungi). The most important factor is the wetland's duration of flooding.[1] Other important factors include fertility and salinity of the water or soils. The chemistry of water flowing into wetlands depends on the source of water, the geological material that it flows through[37] and the nutrients discharged from organic matter in the soils and plants at higher elevations.[38] Plants and animals may vary within a wetland seasonally or in response to flood regimes.

Humid wetland in Pennsylvania before a rain

Flora

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Bud of water lotus (Nelumbo nucifera), an aquatic plant

There are four main groups of hydrophytes that are found in wetland systems throughout the world.[39]

Submerged wetland vegetation can grow in saline and fresh-water conditions. Some species have underwater flowers, while others have long stems to allow the flowers to reach the surface.[40] Submerged species provide a food source for native fauna, habitat for invertebrates, and also possess filtration capabilities. Examples include seagrasses and eelgrass.

Floating water plants or floating vegetation are usually small, like those in the Lemnoideae subfamily (duckweeds). Emergent vegetation like the cattails (Typha spp.), sedges (Carex spp.) and arrow arum (Peltandra virginica) rise above the surface of the water.

When trees and shrubs comprise much of the plant cover in saturated soils, those areas in most cases are called swamps.[1] The upland boundary of swamps is determined partly by water levels. This can be affected by dams[41] Some swamps can be dominated by a single species, such as silver maple swamps around the Great Lakes.[42] Others, like those of the Amazon basin, have large numbers of different tree species.[43] Other examples include cypress (Taxodium) and mangrove swamps.

Fauna

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Many species of frogs live in wetlands, while others visit them each year to lay eggs.
Snapping turtles are one of the many kinds of turtles found in wetlands.

Many species of fish are highly dependent on wetland ecosystems.[44][45] Seventy-five percent of the United States' commercial fish and shellfish stocks depend solely on estuaries to survive.[46]

Amphibians such as frogs and salamanders need both terrestrial and aquatic habitats in which to reproduce and feed. Because amphibians often inhabit depressional wetlands like prairie potholes and Carolina bays, the connectivity among these isolated wetlands is an important control of regional populations.[47] While tadpoles feed on algae, adult frogs forage on insects. Frogs are sometimes used as an indicator of ecosystem health because their thin skin permits absorption of nutrients and toxins from the surrounding environment resulting in increased extinction rates in unfavorable and polluted environmental conditions.[48]

Reptiles such as snakes, lizards, turtles, alligators and crocodiles are common in wetlands of some regions. In freshwater wetlands of the Southeastern US, alligators are common and a freshwater species of crocodile occurs in South Florida. The Florida Everglades is the only place in the world where both crocodiles and alligators coexist.[49] The saltwater crocodile inhabits estuaries and mangroves.[50] Snapping turtles also inhabit wetlands.[51]

Birds, particularly waterfowl and waders use wetlands extensively.[52]

Mammals of wetlands include numerous small and medium-sized species such as voles, bats,[53] muskrats[54] and platypus in addition to large herbivorous and apex predator species such as the beavers,[55] coypu, swamp rabbit, Florida panther,[56] jaguar,[57] and moose. Wetlands attract many mammals due to abundant seeds, berries, and other vegetation as food for herbivores, as well as abundant populations of invertebrates, small reptiles and amphibians as prey for predators.[58]

Invertebrates of wetlands include aquatic insects such as dragonflies, aquatic bugs and beetles, midges, mosquitos, crustaceans such as crabs, crayfish, shrimps, microcrustaceans, mollusks like clams, mussels, snails and worms. Invertebrates comprise more than half of the known animal species in wetlands, and are considered the primary food web link between plants and higher animals (such as fish and birds).[59]

Ecosystem services

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Further information: Ecosystem service

Depending on a wetland's geographic and topographic location,[60] the functions it performs can support multiple ecosystem services, values, or benefits. United Nations Millennium Ecosystem Assessment and Ramsar Convention described wetlands as a whole to be of biosphere significance and societal importance in the following areas:[61]

According to the Ramsar Convention:[citation needed]

The economic worth of the ecosystem services provided to society by intact, naturally functioning wetlands is frequently much greater than the perceived benefits of converting them to 'more valuable' intensive land use – particularly as the profits from unsustainable use often go to relatively few individuals or corporations, rather than being shared by society as a whole.

To replace these wetland ecosystem services, enormous amounts of money would need to be spent on water purification plants, dams, levees, and other hard infrastructure, and many of the services are impossible to replace.

Storage reservoirs and flood protection

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Floodplains and closed-depression wetlands can provide the functions of storage reservoirs and flood protection. The wetland system of floodplains is formed from major rivers downstream from their headwaters. "The floodplains of major rivers act as natural storage reservoirs, enabling excess water to spread out over a wide area, which reduces its depth and speed. Wetlands close to the headwaters of streams and rivers can slow down rainwater runoff and spring snowmelt so that it does not run straight off the land into water courses. This can help prevent sudden, damaging floods downstream."[46]

Notable river systems that produce wide floodplains include the Nile River, the Niger river inland delta, the Zambezi River flood plain, the Okavango River inland delta, the Kafue River flood plain, the Lake Bangweulu flood plain (Africa), Mississippi River (US), Amazon River (South America), Yangtze River (China), Danube River (Central Europe) and Murray-Darling River (Australia).

Groundwater replenishment

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Groundwater replenishment can be achieved for example by marsh, swamp, and subterranean karst and cave hydrological systems. The surface water visibly seen in wetlands only represents a portion of the overall water cycle, which also includes atmospheric water (precipitation) and groundwater. Many wetlands are directly linked to groundwater and they can be a crucial regulator of both the quantity and quality of water found below the ground. Wetlands that have permeable substrates like limestone or occur in areas with highly variable and fluctuating water tables have especially important roles in groundwater replenishment or water recharge.[62]

Substrates that are porous allow water to filter down through the soil and underlying rock into aquifers which are the source of much of the world's drinking water. Wetlands can also act as recharge areas when the surrounding water table is low and as a discharge zone when it is high.

Shoreline stabilization and storm protection

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Main article: Integrated coastal zone management

Mangroves, coral reefs, salt marsh can help with shoreline stabilization and storm protection. Tidal and inter-tidal wetland systems protect and stabilize coastal zones.[63] Coral reefs provide a protective barrier to coastal shoreline. Mangroves stabilize the coastal zone from the interior and will migrate with the shoreline to remain adjacent to the boundary of the water. The main conservation benefit these systems have against storms and storm surges is the ability to reduce the speed and height of waves and floodwaters.

The United Kingdom has begun the concept of managed coastal realignment. This management technique provides shoreline protection through restoration of natural wetlands rather than through applied engineering. In East Asia, reclamation of coastal wetlands has resulted in widespread transformation of the coastal zone, and up to 65% of coastal wetlands have been destroyed by coastal development.[64][65] One analysis using the impact of hurricanes versus storm protection provided naturally by wetlands projected the value of this service at US$33,000/hectare/year.[66]

Water purification

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Water purification can be provided by floodplains, closed-depression wetlands, mudflat, freshwater marsh, salt marsh, mangroves. Wetlands cycle both sediments and nutrients, sometimes serving as buffers between terrestrial and aquatic ecosystems. A natural function of wetland vegetation is the up-take, storage, and (for nitrate) the removal of nutrients found in runoff water from the surrounding landscapes.[67]

Precipitation and surface runoff induces soil erosion, transporting sediment in suspension into and through waterways. All types of sediments whether composed of clay, silt, sand or gravel and rock can be carried into wetland systems through erosion. Wetland vegetation acts as a physical barrier to slow water flow and then trap sediment for both short or long periods of time. Suspended sediment can contain heavy metals that are also retained when wetlands trap the sediment.

The ability of wetland systems to store or remove nutrients and trap sediment is highly efficient and effective but each system has a threshold. An overabundance of nutrient input from fertilizer run-off, sewage effluent, or non-point pollution will cause eutrophication. Upstream erosion from deforestation can overwhelm wetlands making them shrink in size and cause dramatic biodiversity loss through excessive sedimentation load.

Wastewater treatment

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Constructed wetlands are built for wastewater treatment. An example of how a natural wetland is used to provide some degree of sewage treatment is the East Kolkata Wetlands in Kolkata, India. The wetlands cover 125 square kilometres (48 sq mi), and are used to treat Kolkata's sewage. The nutrients contained in the wastewater sustain fish farms and agriculture.

This section is an excerpt from Constructed wetland.[edit]
Constructed wetland in an ecological settlement in Flintenbreite near Lübeck, Germany

A constructed wetland is an artificial wetland to treat sewage, greywater, stormwater runoff or industrial wastewater.[68][69] It may also be designed for land reclamation after mining, or as a mitigation step for natural areas lost to land development. Constructed wetlands are engineered systems that use the natural functions of vegetation, soil, and organisms to provide secondary treatment to wastewater. The design of the constructed wetland has to be adjusted according to the type of wastewater to be treated. Constructed wetlands have been used in both centralized and decentralized wastewater systems. Primary treatment is recommended when there is a large amount of suspended solids or soluble organic matter (measured as biochemical oxygen demand and chemical oxygen demand).[70]

Similar to natural wetlands, constructed wetlands also act as a biofilter and/or can remove a range of pollutants (such as organic matter, nutrients, pathogens, heavy metals) from the water. Constructed wetlands are designed to remove water pollutants such as suspended solids, organic matter and nutrients (nitrogen and phosphorus).[70] All types of pathogens (i.e., bacteria, viruses, protozoans and helminths) are expected to be removed to some extent in a constructed wetland. Subsurface wetlands provide greater pathogen removal than surface wetlands.[70]

Reservoirs of biodiversity

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Wetland systems' rich biodiversity has become a focal point catalysed by the Ramsar Convention and World Wildlife Fund.[71] The impact of maintaining biodiversity is seen at the local level through job creation, sustainability, and community productivity. A good example is the Lower Mekong basin which runs through Cambodia, Laos, and Vietnam, supporting over 55 million people.

A key fish species which is overfished,[72] the Piramutaba catfish, Brachyplatystoma vaillantii, migrates more than 3,300 km (2,100 mi) from its nursery grounds near the mouth of the Amazon River to its spawning grounds in Andean tributaries, 400 m (1,300 ft) above sea level, distributing plant seeds along the route.

Intertidal mudflats have a level of productivity similar to that of some wetlands even while possessing a low number of species. The abundant invertebrates found within the mud are a food source for migratory waterfowl.[73]

Mudflats, saltmarshes, mangroves, and seagrass beds have high levels of both species richness and productivity, and are home to important nursery areas for many commercial fish stocks.

Populations of many species are confined geographically to only one or a few wetland systems, often due to the long period of time that the wetlands have been physically isolated from other aquatic sources. For example, the number of endemic species in the Selenga River Delta of Lake Baikal in Russia classifies it as a hotspot for biodiversity and one of the most biodiverse wetlands in the entire world.[74]

Wetland products

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Wetland at the Broadmoor Wildlife Sanctuary in Massachusetts, United States, in February

Wetlands naturally produce an array of vegetation and other ecological products that can be harvested for personal and commercial use.[75] Many fishes have all or part of their life-cycle occurring within a wetland system. Fresh and saltwater fish are the main source of protein for about one billion people[76] and comprise 15% of an additional 3.5 billion people's protein intake.[77] Another food staple found in wetland systems is rice, a popular grain that is consumed at the rate of one fifth of the total global calorie count. In Bangladesh, Cambodia and Vietnam, where rice paddies are predominant on the landscape, rice consumption reach 70%.[78] Some native wetland plants in the Caribbean and Australia are harvested sustainably for medicinal compounds; these include the red mangrove (Rhizophora mangle) which possesses antibacterial, wound-healing, anti-ulcer effects, and antioxidant properties.[78]

Other mangrove-derived products include fuelwood, salt (produced by evaporating seawater), animal fodder, traditional medicines (e.g. from mangrove bark), fibers for textiles and dyes and tannins.[79]

Additional services and uses of wetlands

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Some types of wetlands can serve as fire breaks that help slow the spread of minor wildfires. Larger wetland systems can influence local precipitation patterns. Some boreal wetland systems in catchment headwaters may help extend the period of flow and maintain water temperature in connected downstream waters.[80] Pollination services are supported by many wetlands which may provide the only suitable habitat for pollinating insects, birds, and mammals in highly developed areas.[81]

Disturbances and human impacts

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See also: Human impacts on the environment

Wetlands, the functions and services they provide as well as their flora and fauna, can be affected by several types of disturbances.[82] The disturbances (sometimes termed stressors or alterations) can be human-associated or natural, direct or indirect, reversible or not, and isolated or cumulative.

Disturbances include exogenous factors such as flooding or drought.[10] Humans are disturbing and damaging wetlands for example by oil and gas extraction, building infrastructure, overgrazing of livestock, overfishing, alteration of wetlands including dredging and draining, nutrient pollution and water pollution.[10][11] Disturbance puts different levels of stress on an environment depending on the type and duration of disturbance.[10]

Predominant disturbances of wetlands include:[83][84]

Disturbances can be further categorized as follows:

  • Minor disturbance: Stress that maintains ecosystem integrity.[10]
  • Moderate disturbance: Ecosystem integrity is damaged but can recover in time without assistance.[10]
  • Impairment or severe disturbance: Human intervention may be needed in order for ecosystem to recover.[10]

Nutrient pollution comes from nitrogen inputs to aquatic systems and have drastically effected the dissolved nitrogen content of wetlands, introducing higher nutrient availability which leads to eutrophication.[85]

Biodiversity loss occurs in wetland systems through land use changes, habitat destruction, pollution, exploitation of resources, and invasive species. For example, the introduction of water hyacinth, a native plant of South America into Lake Victoria in East Africa as well as duckweed into non-native areas of Queensland, Australia, have overtaken entire wetland systems overwhelming the habitats and reducing the diversity of native plants and animals.[citation needed]

Conversion to dry land

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To increase economic productivity, wetlands are often converted into dry land with dykes and drains and used for agricultural purposes. The construction of dykes, and dams, has negative consequences for individual wetlands and entire watersheds.[1]: 497  Their proximity to lakes and rivers means that they are often developed for human settlement.[86] Once settlements are constructed and protected by dykes, the settlements then become vulnerable to land subsidence and ever increasing risk of flooding.[1]: 497  The Mississippi River Delta around New Orleans, Louisiana is a well-known example;[87] the Danube Delta in Europe is another.[88]

Drainage of floodplains

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Drainage of floodplains or development activities that narrow floodplain corridors (such as the construction of levees) reduces the ability of coupled river-floodplain systems to control flood damage. That is because modified and less expansive systems must still manage the same amount of precipitation, causing flood peaks to be higher or deeper and floodwaters to travel faster.

Water management engineering developments in the past century have degraded floodplain wetlands through the construction of artificial embankments such as dykes, bunds, levees, weirs, barrages and dams. All concentrate water into a main channel and waters that historically spread slowly over a large, shallow area are concentrated. Loss of wetland floodplains results in more severe and damaging flooding. Catastrophic human impact in the Mississippi River floodplains was seen in death of several hundred individuals during a levee breach in New Orleans caused by Hurricane Katrina. Human-made embankments along the Yangtze River floodplains have caused the main channel of the river to become prone to more frequent and damaging flooding.[89] Some of these events include the loss of riparian vegetation, a 30% loss of the vegetation cover throughout the river's basin, a doubling of the percentage of the land affected by soil erosion, and a reduction in reservoir capacity through siltation build-up in floodplain lakes.[46]

Overfishing

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Overfishing is a major problem for sustainable use of wetlands. Concerns are developing over certain aspects of farm fishing, which uses natural wetlands and waterways to harvest fish for human consumption. Aquaculture is continuing to develop rapidly throughout the Asia-Pacific region especially in China where 90% of the total number of aquaculture farms occur, contributing 80% of global value.[78] Some aquaculture has eliminated massive areas of wetland through practices such as the shrimp farming industry's destruction of mangroves. Even though the damaging impact of large-scale shrimp farming on the coastal ecosystem in many Asian countries has been widely recognized for quite some time now, it has proved difficult to mitigate since other employment avenues for people are lacking. Also burgeoning demand for shrimp globally has provided a large and ready market.[90]

Conservation

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Main article: Wetland conservation
Fog 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.

Wetlands have historically subjected to large draining efforts for development (real estate or agriculture), and flooding to create recreational lakes or generate hydropower. Some of the world's most important agricultural areas were wetlands that have been converted to farmland.[91][92][93][94] Since the 1970s, more focus has been put on preserving wetlands for their natural functions. Since 1900, 65–70% of the world's wetlands have been lost.[95] In order to maintain wetlands and sustain their functions, alterations and disturbances that are outside the normal range of variation should be minimized.

Balancing wetland conservation with the needs of people

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Wetlands are vital ecosystems that enhance the livelihoods for the millions of people who live in and around them. Studies have shown that it is possible to conserve wetlands while improving the livelihoods of people living among them. Case studies conducted in Malawi and Zambia looked at how dambos – wet, grassy valleys or depressions where water seeps to the surface – can be farmed sustainably. Project outcomes included a high yield of crops, development of sustainable farming techniques, and water management strategies that generate enough water for irrigation.[96]

Ramsar Convention

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Main articles: Ramsar Convention and List of Ramsar wetlands of international importance

The Ramsar Convention (full title: Convention on Wetlands of International Importance, especially as Waterfowl Habitat), is an international treaty designed to address global concerns regarding wetland loss and degradation. The primary purposes of the treaty are to list wetlands of international importance and to promote their wise use, with the ultimate goal of preserving the world's wetlands. Methods include restricting access to some wetland areas, as well as educating the public to combat the misconception that wetlands are wastelands. The Convention works closely with five International Organisation Partners (IOPs). These are: Birdlife International, the IUCN, the International Water Management Institute, Wetlands International and the World Wide Fund for Nature. The partners provide technical expertise, help conduct or facilitate field studies and provide financial support.

Restoration

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Restoration and restoration ecologists intend to return wetlands to their natural trajectory by aiding directly with the natural processes of the ecosystem.[10] These direct methods vary with respect to the degree of physical manipulation of the natural environment and each are associated with different levels of restoration.[10] Restoration is needed after disturbance or perturbation of a wetland.[10] There is no one way to restore a wetland and the level of restoration required will be based on the level of disturbance although, each method of restoration does require preparation and administration.[10]

Levels of restoration

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Factors influencing selected approach may include[10] budget, time scale limitations, project goals, level of disturbance, landscape and ecological constraints, political and administrative agendas and socioeconomic priorities.

Prescribed natural or assisted regeneration

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For this strategy, there is no biophysical manipulation and the ecosystem is left to recover based on the process of succession alone.[10] The focus is to eliminate and prevent further disturbance from occurring and for this type of restoration requires prior research to understand the probability that the wetland will recover naturally. This is likely to be the first method of approach since it is the least intrusive and least expensive although some biophysical non-intrusive manipulation may be required to enhance the rate of succession to an acceptable level.[10] Example methods include prescribed burns to small areas, promotion of site specific soil microbiota and plant growth using nucleation planting whereby plants radiate from an initial planting site,[97] and promotion of niche diversity or increasing the range of niches to promote use by a variety of different species.[10] These methods can make it easier for the natural species to flourish by removing environmental impediments and can speed up the process of succession.

Partial reconstruction

[edit]

For this strategy, a mixture of natural regeneration and manipulated environmental control is used. This may require some engineering, and more intensive biophysical manipulations including ripping of subsoil, agrichemical applications of herbicides or insecticides, laying of mulch, mechanical seed dispersal, and tree planting on a large scale.[10] In these circumstances the wetland is impaired and without human assistance it would not recover within an acceptable period of time as determined by ecologists. Methods of restoration used will have to be determined on a site by site basis as each location will require a different approach based on levels of disturbance and the local ecosystem dynamics.[10]

Complete reconstruction

[edit]
Further information: Constructed wetland

This most expensive and intrusive method of reconstruction requires engineering and ground up reconstruction. Because there is a redesign of the entire ecosystem it is important that the natural trajectory of the ecosystem be considered and that the plant species promoted will eventually return the ecosystem towards its natural trajectory.[10]

In many cases constructed wetlands are often designed to treat stormwater/wastewater runoff. They can be used in developments as part of water-sensitive urban design systems and have benefits such as flood mitigation, removing pollutants, carbon sequestration, providing habitat for wildlife and biodiversity in often highly urbanised and fragmented landscapes.[98]

Traditional knowledge

[edit]

The ideas from traditional ecological knowledge can be applied as a holistic approach to the restoration of wetlands.[99] These ideas focus more on responding to the observations detected from the environment considering that each part of a wetland ecosystem is interconnected. Applying these practices on specific locations of wetlands increase productivity, biodiversity, and improve its resilience. These practices include monitoring wetland resources, planting propagules, and addition of key species in order to create a self-sustaining wetland ecosystem.[100]

Climate change aspects

[edit]

Greenhouse gas emissions

[edit]

In Southeast Asia, peat swamp forests and soils are being drained, burnt, mined, and overgrazed, contributing to climate change.[101] As a result of peat drainage, the organic carbon that had built up over thousands of years and is normally under water is suddenly exposed to the air. The peat decomposes and is converted into carbon dioxide (CO2), which is then released into the atmosphere. Peat fires cause the same process to occur rapidly and in addition create enormous clouds of smoke that cross international borders, which now happens almost yearly in Southeast Asia. While peatlands constitute only 3% of the world's land area, their degradation produces 7% of all CO2 emissions.

This section is an excerpt from Greenhouse gas emissions from wetlands.[edit]
A heat map of the planet showing methane emissions from wetlands from 1980 to 2021

Greenhouse gas emissions from wetlands of concern consist primarily of methane and nitrous oxide emissions. Wetlands are the largest natural source of atmospheric methane in the world, and are therefore a major area of concern with respect to climate change.[102][103][104] Wetlands account for approximately 20–30% of atmospheric methane through emissions from soils and plants, and contribute an approximate average of 161 Tg of methane to the atmosphere per year.[105]

Wetlands are characterized by water-logged soils and distinctive communities of plant and animal species that have adapted to the constant presence of water. This high level of water saturation creates conditions conducive to methane production. Most methanogenesis, or methane production, occurs in oxygen-poor environments. Because the microbes that live in warm, moist environments consume oxygen more rapidly than it can diffuse in from the atmosphere, wetlands are the ideal anaerobic environments for fermentation as well as methanogen activity. However, levels of methanogenesis fluctuates due to the availability of oxygen, soil temperature, and the composition of the soil. A warmer, more anaerobic environment with soil rich in organic matter would allow for more efficient methanogenesis.[106]

Some wetlands are a significant source of methane emissions[107][108] and some are also emitters of nitrous oxide.[109][110] Nitrous oxide is a greenhouse gas with a global warming potential 300 times that of carbon dioxide and is the dominant ozone-depleting substance emitted in the 21st century.[111] Wetlands can also act as a sink for greenhouse gases.[112]

Climate change mitigation

[edit]
Further information: Climate change mitigation § Wetlands, Carbon sequestration § Wetlands, and Blue carbon

Studies have favorably identified the potential for coastal wetlands (also called blue carbon ecosystems) to provide some degree of climate change mitigation in two ways: by conservation, reducing the greenhouse gas emissions arising from the loss and degradation of such habitats, and by restoration, to increase carbon dioxide drawdown and its long-term storage.[113] However, CO2 removal using coastal blue carbon restoration has questionable cost-effectiveness when considered only as a climate mitigation action, either for carbon-offsetting or for inclusion in Nationally Determined Contributions.[113]

When wetlands are restored they have mitigation effects through their ability to sink carbon, converting a greenhouse gas (carbon dioxide) to solid plant material through the process of photosynthesis, and also through their ability to store and regulate water.[114][115]

Wetlands store approximately 44.6 million tonnes of carbon per year globally (estimate from 2003).[116] In salt marshes and mangrove swamps in particular, the average carbon sequestration rate is 210 g CO2 m−2 y−1 while peatlands sequester approximately 20–30 g CO2 m−2 y−1.[116][117]

Coastal wetlands, such as tropical mangroves and some temperate salt marshes, are known to be sinks for carbon that otherwise contribute to climate change in its gaseous forms (carbon dioxide and methane).[118] The ability of many tidal wetlands to store carbon and minimize methane flux from tidal sediments has led to sponsorship of blue carbon initiatives that are intended to enhance those processes.[119][120]

Climate change adaptation

[edit]
Further information: Climate change adaptation

The restoration of coastal blue carbon ecosystems is highly advantageous for climate change adaptation, coastal protection, food provision and biodiversity conservation.[113]

Since the middle of the 20th century, human-caused climate change has resulted in observable changes in the global water cycle.[121]: 85  A warming climate makes extremely wet and very dry occurrences more severe, causing more severe floods and droughts. For this reason, some of the ecosystem services that wetlands provide (e.g. water storage and flood control, groundwater replenishment, shoreline stabilization and storm protection) are important for climate change adaptation measures.[122] In most parts of the world and under all emission scenarios, water cycle variability and accompanying extremes are anticipated to rise more quickly than the changes of average values.[121]: 85 

Valuation

[edit]

The value of a wetland to local communities typically involves first mapping a region's wetlands, then assessing the functions and ecosystem services the wetlands provide individually and cumulatively, and finally evaluating that information to prioritize or rank individual wetlands or wetland types for conservation, management, restoration, or development.[123] Over the longer term, it requires keeping inventories[124] of known wetlands and monitoring a representative sample of the wetlands to determine changes due to both natural and human factors.

Assessment

[edit]

Rapid assessment methods are used to score, rank, rate, or categorize various functions, ecosystem services, species, communities, levels of disturbance, and/or ecological health of a wetland or group of wetlands.[125] This is often done to prioritize particular wetlands for conservation (avoidance) or to determine the degree to which loss or alteration of wetland functions should be compensated, such as by restoring degraded wetlands elsewhere or providing additional protections to existing wetlands. Rapid assessment methods are also applied before and after a wetland has been restored or altered, to help monitor or predict the effects of those actions on various wetland functions and the services they provide. Assessments are typically considered to be "rapid" when they require only a single visit to the wetland lasting less than one day, which in some cases may include interpretation of aerial imagery and geographic information system (GIS) analyses of existing spatial data, but not detailed post-visit laboratory analyses of water or biological samples.

To achieve consistency among persons doing the assessment, rapid methods present indicator variables as questions or checklists on standardized data forms, and most methods standardize the scoring or rating procedure that is used to combine question responses into estimates of the levels of specified functions relative to the levels estimated in other wetlands ("calibration sites") assessed previously in a region.[126] Rapid assessment methods, partly because they often use dozens of indicators pertaining to conditions surrounding a wetland as well as within the wetland itself, aim to provide estimates of wetland functions and services that are more accurate and repeatable than simply describing a wetland's class type.[13] A need for wetland assessments to be rapid arises mostly when government agencies set deadlines for decisions affecting a wetland, or when the number of wetlands needing information on their functions or condition is large.

Inventory

[edit]

Although developing a global inventory of wetlands has proven to be a large and difficult undertaking, many efforts at more local scales have been successful.[127] Current efforts are based on available data, but both classification and spatial resolution have sometimes proven to be inadequate for regional or site-specific environmental management decision making. It is difficult to identify small, long, and narrow wetlands within the landscape. Many of today's remote sensing satellites do not have sufficient spatial and spectral resolution to monitor wetland conditions, although multispectral IKONOS[128] and QuickBird[129] data may offer improved spatial resolutions once it is 4 m or higher. Majority of the pixels are just mixtures of several plant species or vegetation types and are difficult to isolate which translates into an inability to classify the vegetation that defines the wetland. The growing availability of 3D vegetation and topography data from LiDAR has partially addressed the limitation of traditional multispectral imagery, as demonstrated in some case studies across the world.[130]

Monitoring and mapping

[edit]

A wetland needs to be monitored[131] over time to assess whether it is functioning at an ecologically sustainable level or whether it is becoming degraded.[132] Degraded wetlands will suffer a loss in water quality, loss of sensitive species, and aberrant functioning of soil geochemical processes.

Practically, many natural wetlands are difficult to monitor from the ground as they quite often are difficult to access and may require exposure to dangerous plants and animals as well as diseases borne by insects or other invertebrates. Remote sensing such as aerial imagery and satellite imaging[133] provides effective tools to map and monitor wetlands across large geographic regions and over time. Many remote sensing methods can be used to map wetlands. The integration of multi-sourced data such as LiDAR and aerial photos proves more effective at mapping wetlands than the use of aerial photos alone,[130] especially with the aid of modern machine learning methods (e.g., deep learning). Overall, using digital data provides a standardized data-collection procedure and an opportunity for data integration within a geographic information system.

Legislation

[edit]

International efforts

[edit]
This section is an excerpt from Ramsar Convention.[edit]

The Ramsar Convention on Wetlands of International Importance Especially as Waterfowl Habitat is an international treaty for the conservation and sustainable use of Ramsar sites (wetlands).[134] It is also known as the Convention on Wetlands. It is named after the city of Ramsar in Iran, where the convention was signed in 1971.

Every three years, representatives of the contracting parties meet as the Conference of the Contracting Parties (COP), the policy-making organ of the convention which adopts decisions (site designations, resolutions and recommendations) to administer the work of the convention and improve the way in which the parties are able to implement its objectives.[135] In 2022, COP14 was co-held in Wuhan, China, and Geneva, Switzerland.

The Upper Navua Conservation Area Ramsar site in Fiji
Sustainable fishing in India, an example of wise use.

National efforts

[edit]

United States

[edit]

Each country and region tends to have a codified definition of wetlands for legal purposes. In the United States, wetlands are defined as "those areas that are inundated or saturated by surface or groundwater at a frequency and duration sufficient to support, and that under normal circumstances do support, a prevalence of vegetation typically adapted for life in saturated soil conditions. Wetlands generally include swamps, marshes, bogs and similar areas".[136] This definition has been used in the enforcement of the Clean Water Act. Some US states, such as Massachusetts and New York, have separate definitions that may differ from the federal government's.

In the United States Code, the term wetland is defined "as land that (A) has a predominance of hydric soils, (B) is inundated or saturated by surface or groundwater at a frequency and duration sufficient to support a prevalence of hydrophytic vegetation typically adapted for life in saturated soil conditions and (C) under normal circumstances supports a prevalence of such vegetation." Related to these legal definitions, "normal circumstances" are expected to occur during the wet portion of the growing season under normal climatic conditions (not unusually dry or unusually wet) and in the absence of significant disturbance. It is not uncommon for a wetland to be dry for long portions of the growing season. Still, under normal environmental conditions, the soils will be inundated to the surface, creating anaerobic conditions persisting through the wet portion of the growing season.[137]

Canada

[edit]

Examples

[edit]
See also: List of Ramsar Wetlands of International Importance, Mediterranean wetlands, List of Ramsar wetland sites in Pakistan, and List of Ramsar sites in Australia

The world's largest wetlands include the swamp forests of the Amazon River basin, the peatlands of the West Siberian Plain,[5] the Pantanal in South America,[6] and the Sundarbans in the Ganges-Brahmaputra delta.[7]

See also

[edit]

References

[edit]
  1. ^ a b c d e f g h i j k l m Keddy, P.A. (2010). Wetland ecology: principles and conservation (2nd ed.). New York: Cambridge University Press. ISBN 978-0521519403. Archived from the original on 2023-03-17. Retrieved 2020-06-03.
  2. ^ a b c "Official page of the Ramsar Convention". Retrieved 2011-09-25.
  3. ^ Davidson, N.C. (2014). "How much wetland has the world lost? Long-term and recent trends in global wetland area". Marine and Freshwater Research. 65 (10): 934–941. doi:10.1071/MF14173. S2CID 85617334.
  4. ^ "US EPA". 2015. Retrieved 2011-09-25.
  5. ^ a b Fraser, L.; Keddy, P.A., eds. (2005). The World's Largest Wetlands: Their Ecology and Conservation. Cambridge, UK: Cambridge University Press. ISBN 978-0521834049.
  6. ^ a b "WWF Pantanal Programme". Retrieved 2011-09-25.
  7. ^ a b Giri, C.; Pengra, B.; Zhu, Z.; Singh, A.; Tieszen, L.L. (2007). "Monitoring mangrove forest dynamics of the Sundarbans in Bangladesh and India using multi-temporal satellite data from 1973 to 2000". Estuarine, Coastal and Shelf Science. 73 (1–2): 91–100. Bibcode:2007ECSS...73...91G. doi:10.1016/j.ecss.2006.12.019.
  8. ^ Bange, H. W. (2006). "Nitrous oxide and methane in European coastal waters". Estuarine, Coastal and Shelf Science. 70 (3): 361–374. Bibcode:2006ECSS...70..361B. doi:10.1016/j.ecss.2006.05.042.
  9. ^ Thompson, A. J.; Giannopoulos, G.; Pretty, J.; Baggs, E. M.; Richardson, D. J. (2012). "Biological sources and sinks of nitrous oxide and strategies to mitigate emissions". Philosophical Transactions of the Royal Society B. 367 (1593): 1157–1168. doi:10.1098/rstb.2011.0415. PMC 3306631. PMID 22451101.
  10. ^ a b c d e f g h i j k l m n o p q r Clewell, AF; Aronson, J (2013). Ecological restoration (2nd ed.). Washington, DC: Island Press.
  11. ^ a b c Mitsch, William J.; Gosselink, James G. (2007-08-24). Wetlands (4th ed.). New York, NY: John Wiley & Sons. ISBN 978-0-471-69967-5.
  12. ^ Davidson, N.C.; D'Cruz, R. & Finlayson, C.M. (2005). Ecosystems and Human Well-being: Wetlands and Water Synthesis: a report of the Millennium Ecosystem Assessment (PDF). Washington, DC: World Resources Institute. ISBN 978-1-56973-597-8.
  13. ^ a b Dorney, J.; Savage, R.; Adamus, P.; Tiner, R., eds. (2018). Wetland and Stream Rapid Assessments: Development, Validation, and Application. London; San Diego, CA: Academic Press. ISBN 978-0-12-805091-0. OCLC 1017607532.
  14. ^ "Home: Oxford English Dictionary". www.oed.com. Retrieved 2022-07-08.
  15. ^ a b c US EPA, OW (2015-09-18). "What is a Wetland?". US EPA. Retrieved 2022-07-08.
  16. ^ "Glossary of Terms". Carpinteria Valley Water District. Archived from the original on April 25, 2012. Retrieved 2012-05-23.
  17. ^ "Glossary". Mapping2.orr.noaa.gov. Archived from the original on 2012-04-25. Retrieved 2012-05-23.
  18. ^ "Glossary". Alabama Power. Archived from the original on 2012-03-21. Retrieved 2012-05-23.
  19. ^ "The Ramsar 40th Anniversary Message for November". Ramsar. Retrieved 2011-10-10.
  20. ^ Environmental Laboratory. (1987). Corps of Engineers wetlands delineation manual. Tech. Rep. Y‐87–1.
  21. ^ Sharitz, Rebecca R.; Batzer, Darold P.; Pennings, Steven C. (2019-12-31). "Ecology of Freshwater and Estuarine Wetlands: An Introduction". Ecology of Freshwater and Estuarine Wetlands. Berkeley: University of California Press. pp. 1–22. doi:10.1525/9780520959118-003. ISBN 978-0-520-95911-8. S2CID 198427881.
  22. ^ "Wetland Types | Department of Environmental Conservation".
  23. ^ A Directory of Important Wetlands in Australia: Third edition, Chapter 2: Wetland classification system, Criteria for inclusion and Data presentation. Australian Department of the Environment. 2001. Retrieved 30 March 2021.
  24. ^ "NPWRC :: Classification of Wetlands and Deepwater Habitats of the United States". www.fws.gov. Archived from the original on 2014-01-21. Retrieved 2018-07-28.
  25. ^ Watson, G. E. (2006). Big Thicket Plant Ecology: An Introduction. Temple Big Thicket Series #5 (Third ed.). Denton, Texas: University of North Texas Press. ISBN 978-1574412147.
  26. ^ "West Gulf Coastal Plain Seepage Swamp and Baygall". Texas Parks and Wildlife. Ecological Mapping systems of Texas. Archived from the original on 2020-07-10. Retrieved 7 July 2020.
  27. ^ "Peatlands, climate change mitigation and biodiversity conservation | The Convention on Wetlands, The Convention on Wetlands". www.ramsar.org.
  28. ^ "Ramsar Convention Technical Reports".
  29. ^ Richardson, J. L.; Arndt, J. L.; Montgomery, J. A. (2001). "Hydrology of wetland and related soils". In Richardson, J. L.; Vepraskas, M. J. (eds.). Wetland Soils. Boca Raton, FL: Lewis Publishers.
  30. ^ Vitt, D. H.; Chee, W (1990). "The relationships of vegetation to surface water chemistry and peat chemistry in fens of Alberta, Canada". Plant Ecology. 89 (2): 87–106. doi:10.1007/bf00032163. S2CID 25071105.
  31. ^ Silliman, B. R.; Grosholz, E. D.; Bertness, M. D., eds. (2009). Human Impacts on Salt Marshes: A Global Perspective. Berkeley, CA: University of California Press.
  32. ^ Smith, M. J.; Schreiber, E. S. G.; Kohout, M.; Ough, K.; Lennie, R.; Turnbull, D.; Jin, C.; Clancy, T. (2007). "Wetlands as landscape units: spatial patterns in salinity and water chemistry". Wetlands, Ecology & Management. 15 (2): 95–103. Bibcode:2007WetEM..15...95S. doi:10.1007/s11273-006-9015-5. S2CID 20196854.
  33. ^ Ponnamperuma, F. N. (1972). "The chemistry of submerged soils". Advances in Agronomy. 24: 29–96. doi:10.1016/S0065-2113(08)60633-1. ISBN 9780120007240.
  34. ^ Moore, P. A. Jr.; Reddy, K. R. (1994). "Role of Eh and pH on phosphorus geochemistry in sediments of Lake Okeechobee, Florida". Journal of Environmental Quality. 23 (5): 955–964. Bibcode:1994JEnvQ..23..955M. doi:10.2134/jeq1994.00472425002300050016x. PMID 34872208.
  35. ^ Minh, L. Q.; Tuong, T. P.; van Mensvoort, M. E. F.; Bouma, J. (1998). "Soil and water table management effects on aluminum dynamics in an acid sulphate soil in Vietnam". Agriculture, Ecosystems & Environment. 68 (3): 255–262. Bibcode:1998AgEE...68..255M. doi:10.1016/s0167-8809(97)00158-8.
  36. ^ Schlesinger, W. A. (1997). Biogeochemistry: An Analysis of Global Change (2nd ed.). San Diego, CA: Academic Press. ISBN 9780126251555.
  37. ^ Bedford, B. L. (1996). "The need to define hydrologic equivalence at the landscape scale for freshwater wetland mitigation". Ecological Applications. 6 (1): 57–68. Bibcode:1996EcoAp...6...57B. doi:10.2307/2269552. JSTOR 2269552.
  38. ^ Nelson, M. L.; Rhoades, C. C.; Dwire, K. A. (2011). "Influences of Bedrock Geology on Water Chemistry of Slope Wetlands and Headwaters Streams in the Southern Rocky Mountains". Wetlands. 31 (2): 251–261. Bibcode:2011Wetl...31..251N. doi:10.1007/s13157-011-0157-8. S2CID 14521026.
  39. ^ "Blacktown Council wetlands". Archived from the original on 2011-04-10. Retrieved 2011-09-25.
  40. ^ Hutchinson, G. E. (1975). A Treatise on Limnology. Vol. 3: Limnological Botany. New York, NY: John Wiley.
  41. ^ Hughes, F. M. R., ed. (2003). The Flooded Forest: Guidance for policy makers and river managers in Europe on the restoration of floodplain forests. FLOBAR2, Department of Geography, University of Cambridge, Cambridge, UK.
  42. ^ Wilcox, D. A; Thompson, T. A.; Booth, R. K.; Nicholas, J. R. (2007). Lake-level variability and water availability in the Great Lakes. USGS Circular 1311.
  43. ^ Goulding, M. (1980). The Fishes and the Forest: Explorations in Amazonian Natural History. Berkeley, CA: University of California Press.
  44. ^ Colvin, S. A. R.; Sullivan, S. M. P.; Shirey, P. D.; Colvin, R. W.; Winemiller, K. O.; Hughes, R. M.; Fausch, K. D.; Infante, D. M.; Olden, J. D.; Bestgen, K. R.; Danehy, R. J.; Eby, L. (2019). "Headwater Streams and Wetlands are Critical for Sustaining Fish, Fisheries, and Ecosystem Services". Fisheries. 44 (2): 73–91. Bibcode:2019Fish...44...73C. doi:10.1002/fsh.10229. S2CID 92052162.
  45. ^ Sievers, M.; Brown, C. J.; Tulloch, V. J. D.; Pearson, R. M.; Haig, J. A.; Turschwell, M. P.; Connolly, R. M. (2019). "The Role of Vegetated Coastal Wetlands for Marine Megafauna Conservation". Trends in Ecology & Evolution. 34 (9): 807–817. Bibcode:2019TEcoE..34..807S. doi:10.1016/j.tree.2019.04.004. hdl:10072/391960. PMID 31126633. S2CID 164219103.
  46. ^ a b c "Ramsar Convention Ecosystem Services Benefit Factsheets". Retrieved 2011-09-25.
  47. ^ Zamberletti, P.; Zaffaroni, M.; Accatino, F.; Creed, I. F.; De Michele, C. (2018). "Connectivity among wetlands matters for vulnerable amphibian populations in wetlandscapes" (PDF). Ecological Modelling. 384: 119–127. Bibcode:2018EcMod.384..119Z. doi:10.1016/j.ecolmodel.2018.05.008. S2CID 90384249.
  48. ^ "Frogs | Bioindicators". Savethefrogs.com. 2011. Retrieved 2014-01-21.
  49. ^ Mazzotti, F.J.; Best, G.R.; Brandt, L.A.; Cherkiss, M.S.; Jeffery, B.M.; Rice, K.G. (2009). "Alligators and crocodiles as indicators for restoration of Everglades ecosystems". Ecological Indicators. 9 (6): S137−S149. Bibcode:2009EcInd...9.S137M. doi:10.1016/j.ecolind.2008.06.008.
  50. ^ Messel, H. (1981). Surveys of tidal river systems in the Northern Territory of Australia and their crocodile populations. Vol. 1. Pergamon Press.
  51. ^ Piczak, M. L.; Chow-Fraser, P. (2019). "Assessment of critical habitat for common snapping turtles (Chelydra serpentina) in an urbanized coastal wetland". Urban Ecosystems. 22 (3): 525–537. Bibcode:2019UrbEc..22..525P. doi:10.1007/s11252-019-00841-1. S2CID 78091420.
  52. ^ Milton, W. (1999). Wetland birds: habitat resources and conservation implications. Cambridge: Cambridge University Press. ISBN 978-0511011368. OCLC 50984660.
  53. ^ Mas, M.; Flaquer, C.; Rebelo, H.; López-Baucells, A. (2021). "Bats and wetlands: synthesising gaps in current knowledge and future opportunities for conservation". Mammal Review. 51 (3): 369–384. doi:10.1111/mam.12243. S2CID 233974999.
  54. ^ Bomske, C. M.; Ahlers, A. A. (2021). "How do muskrats Ondatra zibethicus affect ecosystems? A review of evidence". Mammal Review. 51 (1): 40–50. doi:10.1111/mam.12218. S2CID 224916636.
  55. ^ Rosell, F.; Bozser, O.; Collen, P.; Parker, H. (2005). "Ecological impact of beavers Castor fiber and Castor canadensis and their ability to modify ecosystems". Mammal Review. 35 (3–4): 248–276. doi:10.1111/j.1365-2907.2005.00067.x. hdl:11250/2438080. ISSN 0305-1838.
  56. ^ Kerk, M.; Onorato, D. P.; Hostetler, J. A.; Bolker, B. M.; Oli, M. K. (2019). "Dynamics, Persistence, and Genetic Management of the Endangered Florida Panther Population". Wildlife Monographs. 203 (1): 3–35. Bibcode:2019WildM.203....3V. doi:10.1002/wmon.1041. S2CID 199641325.
  57. ^ Figel, J. J.; Botero-Cañola, S.; Forero-Medina, G.; Sánchez-Londoño, J. D.; Valenzuela, L.; Noss, R. F. (2019). "Wetlands are keystone habitats for jaguars in an intercontinental biodiversity hotspot". PLOS ONE. 14 (9): e0221705. Bibcode:2019PLoSO..1421705F. doi:10.1371/journal.pone.0221705. PMC 6738587. PMID 31509559.
  58. ^ "Mammals in Wetlands". NSW Environment, Energy and Science. Department of Planning, Industry and Environment. 2020. Retrieved 2021-10-11.
  59. ^ Batzer, D. P.; Rader, R. Ben.; Wissinger, S. A. (1999). Invertebrates in freshwater wetlands of North America: ecology and management. New York: Wiley. ISBN 978-0471292586. OCLC 39747651.
  60. ^ Adamus, P.R. and L.T. Stockwell. 1983. A Method for Wetland Functional Assessment. Vol. I. Critical Review and Evaluation Concepts. FHWA-IP-82-23. Federal Highway Admin., Washington, DC.
  61. ^ Millennium Ecosystem Assessment (2005). Ecosystems and human well-being: wetlands and water synthesis: a report of the Millennium Ecosystem Assessment. Washington, DC: World Resources Institute. ISBN 1-56973-597-2. OCLC 62172810.
  62. ^ van der Kamp, Garth; Hayashi, Masaki (2009-02-01). "Groundwater-wetland ecosystem interaction in the semiarid glaciated plains of North America". Hydrogeology Journal. 17 (1): 203–214. Bibcode:2009HydJ...17..203V. doi:10.1007/s10040-008-0367-1. ISSN 1435-0157. S2CID 129332187.
  63. ^ Costanza, Robert; Anderson, Sharolyn J.; Sutton, Paul; Mulder, Kenneth; Mulder, Obadiah; Kubiszewski, Ida; Wang, Xuantong; Liu, Xin; Pérez-Maqueo, Octavio; Luisa Martinez, M.; Jarvis, Diane; Dee, Greg (2021-09-01). "The global value of coastal wetlands for storm protection". Global Environmental Change. 70: 102328. Bibcode:2021GEC....7002328C. doi:10.1016/j.gloenvcha.2021.102328. hdl:1885/296695. ISSN 0959-3780.
  64. ^ MacKinnon, J.; Verkuil, Y. I.; Murray, N. J. (2012), IUCN situation analysis on East and Southeast Asian intertidal habitats, with particular reference to the Yellow Sea (including the Bohai Sea), Occasional Paper of the IUCN Species Survival Commission No. 47, Gland, Switzerland and Cambridge, UK: IUCN, p. 70, ISBN 9782831712550, archived from the original on 2014-06-24
  65. ^ Murray, N. J.; Clemens, R. S.; Phinn, S. R.; Possingham, H. P.; Fuller, R. A. (2014). "Tracking the rapid loss of tidal wetlands in the Yellow Sea" (PDF). Frontiers in Ecology and the Environment. 12 (5): 267–272. Bibcode:2014FrEE...12..267M. doi:10.1890/130260.
  66. ^ "FAO". Archived from the original on 2007-09-09. Retrieved 2011-09-25.
  67. ^ "Letting Nature Do the Job". Wild.org. 2008-08-01. Archived from the original on 2013-01-13. Retrieved 2012-05-23.
  68. ^ Vymazal, Jan; Zhao, Yaqian; Mander, Ülo (2021-11-01). "Recent research challenges in constructed wetlands for wastewater treatment: A review". Ecological Engineering. 169: 106318. doi:10.1016/j.ecoleng.2021.106318. ISSN 0925-8574.
  69. ^ Arden, S.; Ma, X. (2018-07-15). "Constructed wetlands for greywater recycle and reuse: A review". Science of the Total Environment. 630: 587–599. Bibcode:2018ScTEn.630..587A. doi:10.1016/j.scitotenv.2018.02.218. ISSN 0048-9697. PMC 7362998. PMID 29494968.
  70. ^ a b c Maiga, Y., von Sperling, M., Mihelcic, J. 2017. Constructed Wetlands. In: J.B. Rose and B. Jiménez-Cisneros, (eds) Global Water Pathogens Project. (C. Haas, J.R. Mihelcic and M.E. Verbyla) (eds) Part 4 Management Of Risk from Excreta and Wastewater) Michigan State University, E. Lansing, MI, UNESCO. Material was copied from this source, which is available under a Creative Commons Attribution-ShareAlike 3.0 Unported license.
  71. ^ "What is a wetland? And eight other wetland facts". World Wildlife Fund. Retrieved 2022-11-18.
  72. ^ Prestes, Luiza; Barthem, Ronaldo; Mello-Filho, Adauto; Anderson, Elizabeth; Correa, Sandra B.; Couto, Thiago Belisario D'Araujo; Venticinque, Eduardo; Forsberg, Bruce; Cañas, Carlos; Bentes, Bianca; Goulding, Michael (2022-03-02). Aguirre, Windsor E. (ed.). "Proactively averting the collapse of Amazon fisheries based on three migratory flagship species". PLOS ONE. 17 (3): e0264490. Bibcode:2022PLoSO..1764490P. doi:10.1371/journal.pone.0264490. ISSN 1932-6203. PMC 8890642. PMID 35235610.
  73. ^ Jing, Zhu; Kai, Jing; Xiaojing, Gan; Zhijun, Ma (2007). "Food supply in intertidal area for shorebirds during stopover at Chongming Dongtan, China". Acta Ecologica Sinica. 27 (6): 2149–2159. Bibcode:2007AcEcS..27.2149J. doi:10.1016/S1872-2032(07)60045-6.
  74. ^ Lane, Charles R.; Anenkhonov, Oleg; Liu, Hongxing; Autrey, Bradley C.; Chepinoga, Victor (2015). "Classification and inventory of freshwater wetlands and aquatic habitats in the Selenga River Delta of Lake Baikal, Russia, using high-resolution satellite imagery". Wetlands Ecology and Management. 23 (2): 195–214. Bibcode:2015WetEM..23..195L. doi:10.1007/s11273-014-9369-z. ISSN 0923-4861. S2CID 16980247.
  75. ^ Maltby, E. (1986). Waterlogged wealth: why waste the world's wet places?. Earthscan. London: International Institute for Environment and Development. ISBN 978-0905347639.
  76. ^ Tidwell, James H; Allan, Geoff L (2001). "Fish as food: aquaculture's contribution: Ecological and economic impacts and contributions of fish farming and capture fisheries". EMBO Reports. 2 (11): 958–963. doi:10.1093/embo-reports/kve236. ISSN 1469-221X. PMC 1084135. PMID 11713181.
  77. ^ Béné, Christophe; Barange, Manuel; Subasinghe, Rohana; Pinstrup-Andersen, Per; Merino, Gorka; Hemre, Gro-Ingunn; Williams, Meryl (2015-04-01). "Feeding 9 billion by 2050 – Putting fish back on the menu". Food Security. 7 (2): 261–274. doi:10.1007/s12571-015-0427-z. ISSN 1876-4525. S2CID 18671617.
  78. ^ a b c "The Ramsar Information Sheet on Wetlands of International Importance". September 18, 2009. Retrieved November 19, 2011.
  79. ^ Hogarth, Peter J. (2015). The biology of mangroves and seagrasses (Third ed.). Oxford. ISBN 978-0-19-102590-7. OCLC 907773290.{{cite book}}: CS1 maint: location missing publisher (link)
  80. ^ Leibowitz, Scott G.; Wigington, Parker J.; Schofield, Kate A.; Alexander, Laurie C.; Vanderhoof, Melanie K.; Golden, Heather E. (2018). "Connectivity of Streams and Wetlands to Downstream Waters: An Integrated Systems Framework". JAWRA Journal of the American Water Resources Association. 54 (2): 298–322. Bibcode:2018JAWRA..54..298L. doi:10.1111/1752-1688.12631. PMC 6071435. PMID 30078985.
  81. ^ McInnes, Robert J. (2016), Finlayson, C. Max; Everard, Mark; Irvine, Kenneth; McInnes, Robert J. (eds.), "Managing Wetlands for Pollination", The Wetland Book, Dordrecht: Springer Netherlands, pp. 1–4, doi:10.1007/978-94-007-6172-8_226-1, ISBN 978-94-007-6172-8
  82. ^ Swindles, Graeme T.; Morris, Paul J.; Mullan, Donal J.; Payne, Richard J.; Roland, Thomas P.; Amesbury, Matthew J.; Lamentowicz, Mariusz; Turner, T. Edward; Gallego-Sala, Angela; Sim, Thomas; Barr, Iestyn D. (2019-10-21). "Widespread drying of European peatlands in recent centuries". Nature Geoscience. 12 (11): 922–928. Bibcode:2019NatGe..12..922S. doi:10.1038/s41561-019-0462-z. hdl:10871/39305. ISSN 1752-0908. S2CID 202908362. Alt URL Archived 2020-07-27 at the Wayback Machine
  83. ^ Office of Research & Development. "Impacts on quality of inland wetlands of the United States: A survey of indicators, techniques, and applications of community-level biomonitoring data". cfpub.epa.gov. Retrieved 2018-07-27.
  84. ^ Adamus, Paul; J. Danielson, Thomas; Gonyaw, Alex (2001-03-24). Indicators for Monitoring Biological Integrity of Inland Freshwater Wetlands: A Survey of North American Technical Literature (1990–2000). 13214. doi:10.13140/rg.2.2.22371.86566.
  85. ^ Finlay, Jacques C.; Efi Foufoula-Georgiou; Dolph, Christine L.; Hansen, Amy T. (February 2018). "Contribution of wetlands to nitrate removal at the watershed scale". Nature Geoscience. 11 (2): 127–132. Bibcode:2018NatGe..11..127H. doi:10.1038/s41561-017-0056-6. ISSN 1752-0908. S2CID 46656300.
  86. ^ Alexander, David E. (1 May 1999). Encyclopedia of Environmental Science. Springer. ISBN 0-412-74050-8.
  87. ^ Keddy, P.A.; Campbell, D.; McFalls, T.; Shaffer, G.P.; Moreau, R.; Dranguet, C.; Heleniak, R. (2007). "The Wetlands of Lakes Pontchartrain and Maurepas: Past, Present and Future". Environmental Reviews. 15 (NA): 43–77. doi:10.1139/a06-008. ISSN 1181-8700.
  88. ^ Gastescu, P. (1993). The Danube Delta: geographical characteristics and ecological recovery. Earth and Environmental Science, 29, 57–67.
  89. ^ Li, Luqian; Lu, XiXi; Chen, Zhongyuan (2007). "River channel change during the last 50 years in the middle Yangtze River, the Jianli reach". Geomorphology. 85 (3–4): 185–196. Bibcode:2007Geomo..85..185L. doi:10.1016/j.geomorph.2006.03.035.
  90. ^ "Shrimp Market Size, Share & Growth Analysis Report, 2030". www.grandviewresearch.com. Retrieved 2022-11-19.
  91. ^ Van de Ven, G. P. (2004). Man-Made Lowlands: History of water management and land reclamation in the Netherlands. Utrecht: Uitgeverij Matrijs.
  92. ^ Wells, Samuel A. (1830). A History of the Drainage of the Great Level of the Fens called Bedford Level 2. London: R. Pheney.
  93. ^ Dahl, Thomas E.; Allord, Gregory J. "History of Wetlands in the Conterminous United States".
  94. ^ Lander, Brian (2014). "State Management of River Dikes in Early China: New Sources on the Environmental History of the Central Yangzi Region". T'oung Pao. 100 (4–5): 325–362. doi:10.1163/15685322-10045p02.
  95. ^ Davidson, Nick C. (2014). "How much wetland has the world lost? Long-term and recent trends in global wetland area". Marine and Freshwater Research. 65 (10): 934. doi:10.1071/MF14173. ISSN 1323-1650.
  96. ^ "Good practices and lessons learned in integrating ecosystem conservation and poverty reduction objectives in wetlands". The Ramsar Convention on Wetlands. 2008-12-01. Retrieved 10 May 2022.
  97. ^ Corbin, JD; Holl, KD (2012). "Applied nucleation as a forest restoration strategy". Forest Ecology and Management. 256: 37–46. Bibcode:2012ForEM.265...37C. doi:10.1016/j.foreco.2011.10.013.
  98. ^ Functional assessment of wetlands: towards evaluation of ecosystem services. Cambridge: Woodhead Publ. [u.a.] 2009. ISBN 978-1-84569-516-3.
  99. ^ Inglis, J. T. (1993). Traditional Ecological Knowledge: Concepts and Cases. Ottawa, Canada: International Program on Traditional Ecological and International Development Research Centre. ISBN 978-0-88936-683-1.
  100. ^ Craft, Christopher (2022-05-12). Creating and Restoring Wetlands: From Theory to Practice. Elsevier. ISBN 978-0-12-823982-7.
  101. ^ "Wetlands International works to sustain and restore wetlands for people and biodiversity". Wetlands International. Retrieved 2014-01-21.
  102. ^ Houghton, J. T., et al. (Eds.) (2001) Projections of future climate change, Climate Change 2001: The Scientific Basis, Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change, 881 pp.
  103. ^ Comyn-Platt, Edward (2018). "Carbon budgets for 1.5 and 2 °C targets lowered by natural wetland and permafrost feedbacks" (PDF). Nature. 11 (8): 568–573. Bibcode:2018NatGe..11..568C. doi:10.1038/s41561-018-0174-9. S2CID 134078252.
  104. ^ Bridgham, Scott D.; Cadillo-Quiroz, Hinsby; Keller, Jason K.; Zhuang, Qianlai (May 2013). "Methane emissions from wetlands: biogeochemical, microbial, and modeling perspectives from local to global scales". Global Change Biology. 19 (5): 1325–1346. Bibcode:2013GCBio..19.1325B. doi:10.1111/gcb.12131. PMID 23505021. S2CID 14228726.
  105. ^ Saunois, Marielle; Stavert, Ann R.; Poulter, Ben; Bousquet, Philippe; Canadell, Josep G.; Jackson, Robert B.; Raymond, Peter A.; Dlugokencky, Edward J.; Houweling, Sander; Patra, Prabir K.; Ciais, Philippe; Arora, Vivek K.; Bastviken, David; Bergamaschi, Peter; Blake, Donald R. (2020-07-15). "The Global Methane Budget 2000–2017". Earth System Science Data. 12 (3): 1561–1623. doi:10.5194/essd-12-1561-2020. hdl:1721.1/124698. ISSN 1866-3508.
  106. ^ Christensen, T. R., A. Ekberg, L. Strom, M. Mastepanov, N. Panikov, M. Oquist, B. H. Svenson, H. Nykanen, P. J. Martikainen, and H. Oskarsson (2003), Factors controlling large scale variations in methane emissions from wetlands, Geophys. Res. Lett., 30, 1414, doi:10.1029/2002GL016848.
  107. ^ Masso, Luana S.; Marani, Luciano; Gatti, Luciana V.; Miller, John B.; Gloor, Manuel; Melack, John; Cassol, Henrique L. G.; Tejada, Graciela; Domingues, Lucas G.; Arai, Egidio; Sanchez, Alber H.; Corrêa, Sergio M.; Anderson, Liana; Aragão, Luiz E. O. C.; Correa, Caio S. C.; Crispim, Stephane P.; Neves, Raiane A. L. (29 November 2021). "Amazon methane budget derived from multi-year airborne observations highlights regional variations in emissions". Communications Earth & Environment. 2 (1): 246. Bibcode:2021ComEE...2..246B. doi:10.1038/s43247-021-00314-4. S2CID 244711959.
  108. ^ Tiwari, Shashank; Singh, Chhatarpal; Singh, Jay Shankar (2020). "Wetlands: A Major Natural Source Responsible for Methane Emission". In Upadhyay, Atul Kumar; Singh, Ranjan; Singh, D. P. (eds.). Restoration of Wetland Ecosystem: A Trajectory Towards a Sustainable Environment. Singapore: Springer. pp. 59–74. doi:10.1007/978-981-13-7665-8_5. ISBN 978-981-13-7665-8. S2CID 198421761.
  109. ^ Bange, Hermann W. (2006). "Nitrous oxide and methane in European coastal waters". Estuarine, Coastal and Shelf Science. 70 (3): 361–374. Bibcode:2006ECSS...70..361B. doi:10.1016/j.ecss.2006.05.042.
  110. ^ Thompson, A. J.; Giannopoulos, G.; Pretty, J.; Baggs, E. M.; Richardson, D. J. (2012). "Biological sources and sinks of nitrous oxide and strategies to mitigate emissions". Philosophical Transactions of the Royal Society B. 367 (1593): 1157–1168. doi:10.1098/rstb.2011.0415. PMC 3306631. PMID 22451101.
  111. ^ Ravishankara, A. R.; Daniel, John S.; Portmann, Robert W. (2009). "Nitrous Oxide (N2O): The Dominant Ozone-Depleting Substance Emitted in the 21st Century". Science. 326 (5949): 123–125. Bibcode:2009Sci...326..123R. doi:10.1126/science.1176985. PMID 19713491. S2CID 2100618.
  112. ^ Sonwani, Saurabh; Saxena, Pallavi (2022-01-21). Greenhouse Gases: Sources, Sinks and Mitigation. Springer Nature. pp. 47–48. ISBN 978-981-16-4482-5.
  113. ^ a b c Williamson, Phillip; Gattuso, Jean-Pierre (2022). "Carbon Removal Using Coastal Blue Carbon Ecosystems Is Uncertain and Unreliable, With Questionable Climatic Cost-Effectiveness". Frontiers in Climate. 4: 853666. doi:10.3389/fclim.2022.853666. ISSN 2624-9553. Text was copied from this source, which is available under a Creative Commons Attribution 4.0 International License Archived 2017-10-16 at the Wayback Machine
  114. ^ Synthesis of Adaptation Options for Coastal Areas. Climate Ready Estuaries Program, EPA 430-F-08-024. Washington, DC: US Environmental Protection Agency. 2009.
  115. ^ "Coastal Wetland Protection". Project Drawdown. 2020-02-06. Retrieved 2020-09-13.
  116. ^ a b Chmura, G. L. (2003). "Global carbon sequestration in tidal, saline wetland soils". Global Biogeochemical Cycles. 17 (4): 1111. Bibcode:2003GBioC..17.1111C. doi:10.1029/2002GB001917. S2CID 36119878.[page needed]
  117. ^ Roulet, N. T. (2000). "Peatlands, Carbon Storage, Greenhouse Gases, And The Kyoto Protocol: Prospects And Significance For Canada". Wetlands. 20 (4): 605–615. doi:10.1672/0277-5212(2000)020[0605:pcsgga]2.0.co;2. S2CID 7490212.
  118. ^ Ouyang, Xiaoguang; Lee, Shing Yip (2020-01-16). "Improved estimates on global carbon stock and carbon pools in tidal wetlands". Nature Communications. 11 (1): 317. Bibcode:2020NatCo..11..317O. doi:10.1038/s41467-019-14120-2. ISSN 2041-1723. PMC 6965625. PMID 31949151.
  119. ^ "Blue Carbon". Earth Times.
  120. ^ Wang, F. (2021). "Global blue carbon accumulation in tidal wetlands increases with climate change". National Science Review. 8 (9): nwaa296. doi:10.1093/nsr/nwaa296. PMC 8433083. PMID 34691731.
  121. ^ a b Arias, P.A., N. Bellouin, E. Coppola, R.G. Jones, G. Krinner, J. Marotzke, V. Naik, M.D. Palmer, G.-K. Plattner, J. Rogelj, M. Rojas, J. Sillmann, T. Storelvmo, P.W. Thorne, B. Trewin, K. Achuta Rao, B. Adhikary, R.P. Allan, K. Armour, G. Bala, R. Barimalala, S. Berger, J.G. Canadell, C. Cassou, A. Cherchi, W. Collins, W.D. Collins, S.L. Connors, S. Corti, F. Cruz, F.J. Dentener, C. Dereczynski, A. Di Luca, A. Diongue Niang, F.J. Doblas-Reyes, A. Dosio, H. Douville, F. Engelbrecht, V.  Eyring, E. Fischer, P. Forster, B. Fox-Kemper, J.S. Fuglestvedt, J.C. Fyfe, et al., 2021: Technical Summary Archived 2022-07-21 at the Wayback Machine. In Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change Archived 2021-08-09 at the Wayback Machine [Masson-Delmotte, V., P. Zhai, A. Pirani, S.L. Connors, C. Péan, S. Berger, N. Caud, Y. Chen, L. Goldfarb, M.I. Gomis, M. Huang, K. Leitzell, E. Lonnoy, J.B.R. Matthews, T.K. Maycock, T. Waterfield, O. Yelekçi, R. Yu, and B. Zhou (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp. 33–144. doi:10.1017/9781009157896.002.
  122. ^ "Fact Sheet: Blue Carbon". American University. Archived from the original on April 28, 2021. Retrieved 2021-04-28.
  123. ^ Emerton, Lucy (2016), Finlayson, C. Max; Everard, Mark; Irvine, Kenneth; McInnes, Robert J. (eds.), "Economic Valuation of Wetlands: Total Economic Value", The Wetland Book, Dordrecht: Springer Netherlands, pp. 1–6, doi:10.1007/978-94-007-6172-8_301-1, ISBN 978-94-007-6172-8
  124. ^ "A new toolkit for National Wetlands Inventories | Convention on Wetlands". www.ramsar.org. Retrieved 2022-11-28.
  125. ^ McInnes, R.J.; Everard, M. (2017). "Rapid Assessment of Wetland Ecosystem Services (RAWES): An example from Colombo, Sri Lanka". Ecosystem Services. 25: 89–105. Bibcode:2017EcoSv..25...89M. doi:10.1016/j.ecoser.2017.03.024. S2CID 56403914.
  126. ^ Adamus, P. (2016). "Manual for the Wetland Ecosystem Services Protocol (WESP)" (PDF). Oregon State University. Archived (PDF) from the original on 2018-07-28. Retrieved July 28, 2018.
  127. ^ "Home | Ramsar Sites Information Service". rsis.ramsar.org. Retrieved 2022-11-28.
  128. ^ Wei, Anhua; Chow-Fraser, Patricia (2007). "Use of IKONOS Imagery to Map Coastal Wetlands of Georgian Bay". Fisheries. 32 (4): 167–173. doi:10.1577/1548-8446(2007)32[167:UOIITM]2.0.CO;2. ISSN 0363-2415.
  129. ^ Cook, Bruce D.; Bolstad, Paul V.; Næsset, Erik; Anderson, Ryan S.; Garrigues, Sebastian; Morisette, Jeffrey T.; Nickeson, Jaime; Davis, Kenneth J. (2009-11-16). "Using LiDAR and quickbird data to model plant production and quantify uncertainties associated with wetland detection and land cover generalizations". Remote Sensing of Environment. 113 (11): 2366–2379. Bibcode:2009RSEnv.113.2366C. doi:10.1016/j.rse.2009.06.017.
  130. ^ a b Xu, Haiqing; Toman, Elizabeth; Zhao, Kaiguang; Baird, John (2022). "Fusion of Lidar and Aerial Imagery to Map Wetlands and Channels via Deep Convolutional Neural Network". Transportation Research Record. 2676 (12): 374–381. doi:10.1177/03611981221095522. S2CID 251780248.
  131. ^ Stephenson, P. J.; Ntiamoa-Baidu, Yaa; Simaika, John P. (2020). "The Use of Traditional and Modern Tools for Monitoring Wetlands Biodiversity in Africa: Challenges and Opportunities". Frontiers in Environmental Science. 8. doi:10.3389/fenvs.2020.00061. ISSN 2296-665X.
  132. ^ Bhatnagar, Saheba; Gill, Laurence; Regan, Shane; Waldren, Stephen; Ghosh, Bidisha (2021-04-01). "A nested drone-satellite approach to monitoring the ecological conditions of wetlands". ISPRS Journal of Photogrammetry and Remote Sensing. 174: 151–165. Bibcode:2021JPRS..174..151B. doi:10.1016/j.isprsjprs.2021.01.012. ISSN 0924-2716. S2CID 233522024.
  133. ^ Munizaga, Juan; García, Mariano; Ureta, Fernando; Novoa, Vanessa; Rojas, Octavio; Rojas, Carolina (2022). "Mapping Coastal Wetlands Using Satellite Imagery and Machine Learning in a Highly Urbanized Landscape". Sustainability. 14 (9): 5700. doi:10.3390/su14095700. ISSN 2071-1050.
  134. ^ "The Ramsar Convention and its Mission". Archived from the original on 9 April 2016. Retrieved 11 October 2016.
  135. ^ "The Conference of the Contracting Parties". Ramsar. Retrieved 31 March 2019.
  136. ^ "EPA Regulations listed at 40 CFR 230.3(t)". US Environmental Protection Agency. March 2015. Retrieved 2014-02-18.
  137. ^ US Government Publishing Office. (2011) 16 U.S. Code Chapter 58 Subchapter I, § 3801 – Definitions Archived 2017-02-06 at the Wayback Machine. Legal Information Institute, Cornell Law School, Ithaca.
  138. ^ a b Rubec, C. D.A.; Hanson, A. R (2009). "Wetland mitigation and compensation: Canadian experience". Wetlands Ecol Manage. 17 (1): 3–14. Bibcode:2009WetEM..17....3R. doi:10.1007/s11273-008-9078-6. S2CID 32876048.
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