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Peat swamp forests aretropical moist forests where waterlogged soil prevents dead leaves and wood from fully decomposing. Over time, this creates a thick layer of acidicpeat.[1] Large areas of these forests are being logged at high rates.
Peat swamp forests are typically surrounded by lowland rain forests on better-drained soils, and bybrackish or salt-watermangrove forests near the coast.
They are a kind ofpeatland, which store and accumulate vast amounts of carbon assoil organic matter—much more than forests on mineral soil (i.e. non-peatland) contain. Peat formation is a naturalcarbon sink; because the decomposition of the organic matter is slower than its production rate, the surplus accumulates as peat. Their stability has important implications forclimate change; they are among the largest near-surface reserves of terrestrial organic carbon.[2] Tropical peat swamp forests, which have ecological importance, are one of the most threatened, yet least studied and most poorly understood biotypes.
Since the 1970s, tropical peat swamp forestdeforestation anddrainage have greatly increased in South East Asia.[3] In addition,El Niño Southern Oscillation (ENSO) drought and large-scale fires are accelerating peatland devastation. Peat fires, drainage and deforestation enhances the decomposition of soil organic matter, increasing the release of stored carbon into the atmosphere ascarbon dioxide.[4]
Tropical peat swamp forests are home to thousands of animals and plants, including many rare and critically endangered species such as theorangutan andSumatran tiger, whose habitats are threatened by peatland deforestation.[5]
Tropical peat ecosystem are found in three regions: Central America, Africa and South East Asia.[2] About 62% of the world's tropical peat lands occur in theIndomalayan realm (80% inIndonesia, 11% inMalaysia, 6% inPapua New Guinea, and pockets inBrunei,Vietnam, thePhilippines, andThailand).[6][7] Peat in Indonesia is distributed over three islands, Sumatra (8.3 million ha), Kalimantan (6.3 million ha) and Papua (4.6 million ha).[8] 36% of the world's tropical peat occurs in Africa's central Congo Basin.[9]
Tropical peat forms on low-lying areas, such asriver deltas,floodplains or shallowoxbow lakes. The formation process usually followshydroseresuccessional steps,[1][10] where the ponds or flooded areaeutrophicated by water plants, then transform into waterlogged swamp with grasses or shrubs, and eventually formed a forest that continues to grow and accumulate.[10] Peat located on the fringing areas of domes in between domes might form through lateral expansion.[10][11] This peat accumulation often forms a convex shape called a dome, which could rise up to 4 m (13 ft) on coastal peat and up to 18 m (59 ft) on inland peat.[1] At the beginning of its formation, peat is largely topogenous or minerotrophic, receiving high nutrient input from rivers orgroundwaters. As the peat thickens and the dome becomes elevated, the top of the peat is no longer affected by the river or groundwater input, instead they are becomingombrotrophic, exclusively obtaining water from the precipitation[8][10] Input only from the rain causes a low nutrient and mineral content, especially calcium. The peat thus becomes highly acidic and only able to support low biodiversity and stunted forest.
Inland and coastal peat differ greatly in their age, where coastal peat formed during the midHolocene, about 8000 years ago.[12] Inland peat formed much earlier during theLate Pleistocene, more than 26000 BP.[13] Coastal peat formation is highly affected by thesea level rise with strong accumulation around 8-4000 BP whenEl Niño is less intense.[14] Because theSunda Shelf is tectonically stable, the sea level change in this area is only affected by the eustaticsea level, and during the glacial period theKarimata Strait dried, causing Asian Peninsula,Sumatra,Borneo andJava to become connected.[15] After theLast Glacial Maximum, this coastline moved inland as the ice sheet melted, and finally reached the level of modern coastline around 8500 BP. Thus, the oldest age of coastal peat in this region is less than 8500 years old.[16]
Inland peat formation is highly affected by climate with little or no effect of sea level rise because it located around 15–20 m (49–66 ft) above sea level, where the most recent record of higher sea level was during about 125000 BP when sea level was 6 m above the modern level.[17] Peat cores fromSebangau,South Kalimantan show a slow growth of 0.04 mm/y around 13000 BP when the climate was colder, then accelerated to 2.55mm/y around 9900 BP in warmer Early Holocene, then slower again to 0.23–0.15 mm/y during intense El Nino.[18] A similar pattern is observed in cores from Sentarum,West Kalimantan, where the peat shows slower growth around 28-16000 BP, 13-3000 BP and on 5-3000 BP.[19] While the slower growth from 28 to 16000 BP and 5-3000 BP is explained by a drier climate during this period due toHeinrich Event I and the emergence ofEl Niño.[20][21]
Peat swamp forest are unusual ecosystems, with trees reaching as high in 70 m (230 ft) in South East Asian ecoregions—vastly different from the peatlands of the north temperate and boreal zones (which are dominated bySphagnum mosses, grasses, sedges and shrubs).[10] The spongy, unstable, waterlogged, anaerobic beds of peat can be up to 20 m (66 ft) deep with lowpH (pH 2.9 – 4) and low nutrients, and the forest floor is seasonally flooded.[22] The water is stained dark brown by thetannins that leach from the fallen leaves and peat – hence the nameblackwater swamps. During the dry season, the peat remains waterlogged and pools remain among the trees. Water level on the peat is usually 20 cm (7.9 in) below the surface.[1] however, during a severe El Nino, this water level might drop to 40 cm (16 in) below the surface and increase the risk of burning.[12]
Peat forest contains high amount of carbon due to its soil nature, categorized ashistosols with characteristics of high organic material content (70–99%).[10][23] This carbon pool is stabilized by the low temperature on temperate peat, and by the water logging on tropical peat. Disturbances that change the temperature or the water content of the peat will release this stored carbon into the atmosphere, exacerbating human-made climate change.[14] Estimation of carbon content of tropical peat ranges from 50 Gt carbon[14] to 88 Gt carbon.[2]
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Peat swamp forests originally represented major ecosystems in Indonesia and ranged between 16.5 and 27 million hectares. In their original state, Indonesian peat swamp forests released between 0.01 and 0.03 Gt of carbon annually. In recent years, however, these important ecosystems have been reduced through deforestation, drainage, and conversion to agricultural lands and other activities. Their current status ascarbon sequestering systems have thus also been reduced significantly. An understanding of the global importance of peat (and thus the urgency of maintaining peat swamp forests) and identifying alternative ways of making these areas productive in an environmentally sound and sustainable manner should have high priority among scientists and policy-makers alike.[24]
Over the past decade, under theMega Rice Project (MRP), the government of Indonesia has drained over 1 million hectares of theBorneo peat swamp forests for conversion to agricultural land. Between 1996 and 1998, more than 4,000 kilometers of drainage and irrigation channels were dug, and deforestation accelerated in part through legal andillegal logging and in part through burning. The water channels, and the roads and railways built for legal forestry, opened up the region to illegal forestry. In the MRP area, forest cover dropped from 64.8% in 1991 to 45.7% in 2000, and clearance has continued since then. It appears that almost all the marketable trees have now been removed from the areas covered by the MRP. What happened was not what had been expected: the channels drained the peat forests rather than irrigating them. Where the forests had often flooded up to 2 meters deep in the rainy season, now their surface is dry at all times of the year. The Indonesian government has now abandoned the MRP.
A study for theEuropean Space Agency found that up to 2.57 billion tons of carbon were released to the atmosphere in 1997 as a result of burning peat and vegetation in Indonesia. This is equivalent to 40% of the average annual global carbon emissions from fossil fuels, and contributed greatly to the largest annual increase in atmospheric CO2 concentration detected since records began in 1957.[25] Additionally, the 2002–03 fires released between 200 million to 1 billion tons of carbon into the atmosphere.
Indonesia is currently the world's third largest carbon emitter, to a large extent due to the destruction of its ancient peat swamp forests.
Indonesia contains 50% of tropical peat swamps and 10% of dry land in the world. They have the potential of playing an important role in mitigating global warming and climate change under thereducing emissions from deforestation and forest degradation (REDD) scheme. Rather than reducing deforestation—in terms of claiming carbon credits from REDD initiatives—peatland conservation and rehabilitation are more efficient undertakings, due to the much larger reduced emissions achievable per unit area and the much lower opportunity costs involved.[26]
Attempts to preserve tropical peat swamp forests have been minimal in comparison to the widespread impact and devastation of commercial logging; in Sarawak, logging is ongoing and planned to intensify in Brunei. One plan by the environmental NGOBorneo Orangutan Survival is to preserve the peat swamp forest ofMawas using a combination ofcarbon finance anddebt-for-nature-swap. About 6% of the original peat-forest area is contained within protected areas, the largest of which areTanjung Puting andSabangau National Parks.
The main causes of deforestation inIndonesia continue to bepalm oil business (seepalm oil production in Indonesia) and illegal logging, ongoing in areas such as South Sumatra. A survey by the University of Muhammadiyah Palembang in 2008 estimated that in 25 years most of the natural forests will be depleted due to illegal logging. Projects by REDD are designed to tackle deforestation and protect forests from the encroachment of agriculture, benefitting biodiversity and improving the quality of the environment to surrounding villages.[27]
To counter the destruction ofmangroves and unsustainable palm oil expansion in Indonesia's peatlands, organizations, such asWetlands International, work with the Indonesian government to improve policies and spatial planning. They engage with the palm-oil industry, promoting best management practices in tropical peat swamp forests and ensuring the participation of local communities, who lack awareness about natural resource management. In the field, they work with communities to restore mangroves and peatlands.
Habitat disturbance caused by logging was shown to affect orangutan density within a mixed swamp forest. The presence of a very large, self-sustaining orangutan population in this region emphasizes the urgency for greater protection ofKalimantan's peat swamp forests in light of recent and rapid habitat degradation.[28]
It has long been assumed that the peat underlying tropical peat swamp forests accumulates because the extreme conditions (waterlogged, nutrient poor, anaerobic and acidic) impede microbial activity. Studies in a tropical Malaysian peat swamp (North Selangor peat swamp forest) showed that although thesclerophyllous, toxic leaves of endemic peat-forest plants (Macaranga pruinosa,Campnosperma coriaceum,Pandanus atrocarpus,Stenochlaena palustris) were barely decomposed by bacteria and fungi, the leaves ofM. tanarius, another plant species, were almost completely decomposed after one year. Thus it is intrinsic properties of the leaves (that are adaptations to deter herbivory in the nutrient poor environment) that impede microbial breakdown.[29]
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