Borneo peat swamp forests

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Borneo peat swamp forests
Peat Forest Swamp (10712654875).jpg
Peat swamp forest in Kalimantan
Ecoregion IM0104.png
Ecoregion territory (in purple)
Ecology
Realm Indomalayan
Biome tropical and subtropical moist broadleaf forests
Borders Borneo lowland rain forests, Southwest Borneo freshwater swamp forests, Sunda Shelf mangroves, and Sundaland heath forests
Geography
Area66,976 km2 (25,860 sq mi)
Countries Brunei, Indonesia, and Malaysia
Conservation
Conservation status critical/endangered
Protected9,144 km² (14%) [1]

The Borneo peat swamp forests ecoregion, within the tropical and subtropical moist broadleaf forests biome, are on the island of Borneo, which is divided between Brunei, Indonesia and Malaysia.

Contents

Location and description

Peat swamp forests occur where waterlogged soils prevent dead leaves and wood from fully decomposing, which over time creates thick layer of acidic peat. The peat swamp forests on Borneo occur in the Indonesian state of Kalimantan, the Malaysian state of Sarawak and in the Belait District of Brunei on coastal lowlands, built up behind the brackish mangrove forests and bounded by the Borneo lowland rain forests on better-drained soils. There are also areas of inland river-fed peat forest at higher elevations in central Kalimantan around the Mahakam Lakes and Lake Sentarum on the Kapuas River. [2] Borneo has a tropical monsoon climate.

Recent history

Over the past decade, the government of Indonesia has drained over 1 million hectares of the Borneo peat swamp forests for conversion to agricultural land under the Mega Rice Project (MRP). Between 1996 and 1998, more than 4,000 km of drainage and irrigation channels were dug, and deforestation accelerated in part through legal and illegal 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 2m deep in the rainy season, now their surface is dry at all times of the year. The Indonesian government has now abandoned the MRP.

Fires

Fires were used in an attempt to create agricultural lands, including large palm tree plantations to supply palm oil. The dried-out peat ignites easily and also burns underground, travelling unseen beneath the surface to break out in unexpected locations. Therefore, after drainage, fires ravaged the area, destroying remaining forest and large numbers of birds, animals, reptiles and other wildlife along with new agriculture, even damaging nature reserves such as Muara Kaman [3] and filling the air above Borneo and beyond with dense smoke and haze and releasing enormous quantities of CO2 into the atmosphere. The destruction had a major negative impact on the livelihoods of people in the area. It caused major smog-related health problems amongst half a million people, who suffered from respiratory problems. [4]

The dry years of 1997-8 and 2002-3 (see El Niño) in particular saw huge fires in the drained and drying-out peat swamp forests. A study for the European Space Agency found that the peat swamp forests are a significant carbon sink for the planet, and that the fires of 1997-8 may have released up to 2.5 billion tonnes, and the 2002-3 fires between 200 million to 1 billion tonnes, of carbon into the atmosphere. [5] Using satellite images from before and after the 1997 fires, scientists calculated (Page et al, 2002) that of the 790,000 hectares (2,000,000 acres) that had burned 91.5% was peatland 730,000 hectares (1,800,000 acres). Using ground measurements of the burn depth of peat, they estimated that 0.19–0.23 gigatonnes (Gt) of carbon were released into the atmosphere through peat combustion, with a further 0.05 Gt released from burning of the overlying vegetation. Extrapolating these estimates to Indonesia as a whole, they estimated that between 0.81 and 2.57 Gt of carbon were released to the atmosphere in 1997 as a result of burning peat and vegetation in Indonesia. This is equivalent to 13–40% of the mean 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.

Indonesia is currently the world's third largest carbon emitter, to a large extent due to the destruction of its ancient peat swamp forests (Pearce 2007).

Ecology

Peat swamp forest in Kalimantan 2007-09-20-57-kalimantan-foresta.jpg
Peat swamp forest in Kalimantan

About 62% of the world's tropical peat lands occur in the Indo-Malayan region (80% in Indonesia, 11% in Malaysia, 6% in Papua New Guinea, with small pockets and remnants in Brunei, Vietnam, the Philippines and Thailand). [6] [7] They are unusual ecosystems, with trees up to 70 m high - vastly different from the peat lands of the north temperate and boreal zones (which are dominated by Sphagnum mosses, grasses, sedges and shrubs). The spongy, unstable, waterlogged, anaerobic beds of peat can be up to 20 m deep with low pH (pH 2.9 – 4) and low nutrients, and the forest floor is seasonally flooded. [8] The water is stained dark brown by the tannins that leach from the fallen leaves and peat – hence the name 'blackwater swamps'. During the dry season, the peat remains waterlogged and pools remain among the trees.

Despite the extreme conditions the Borneo peat swamp forests have as many as 927 species of flowering plants and ferns recorded [9] (In comparison, a biodiversity study in the Pekan peat swamp forest in Peninsular Malaysia reported 260 plant species). [10] Patterns of forest type can be seen in circles from the centre of the swamps to their outer fringes which are made up of most of the tree families recorded in lowland dipterocarp forests although many species are only found here [ citation needed ]. Many trees have buttresses and stilt roots for support in the unstable substrate, and pneumatophores and hoop roots and knee roots to facilitate gas exchange. The trees have thick, root mats in the upper 50 cm of the peat to enable oxygen and nutrient uptake.

Peat swamp forest in Gunung Mulu National Park with Nepenthes bicalcarata in the foreground Headhunter's trail Mulu N. bicalcarata 3.jpg
Peat swamp forest in Gunung Mulu National Park with Nepenthes bicalcarata in the foreground

The lowland peat swamps of Borneo are mostly geologically recent (<5,000 years old), low-lying coastal formations above marine muds and sands [11] [7] but some of the lakeside peat forests of Kalimantan are up to 11,000 years old.

One reason for the low nutrient conditions is that streams and rivers do not flow into these forests (if they did, nutrient rich freshwater swamps would result), water only flows out of them, so the only input of nutrients is from rainfall, marine aerosols and dust. In order to cope with the lack of nutrients, the plants invest heavily in defences against herbivores such as chemical (toxic secondary compounds) and physical defences (tough leathery leaves, spines and thorns). It is these defences that prevent the leaves from decaying and so they build up as peat. Although the cellular contents quickly leach out of the leaves when they fall, the physical structure is resistant to both bacterial and fungal decomposition and so remains intact, slowly breaking down to form peat (Yule and Gomez 2008). This is in stark contrast to the lowland dipterocarp forests where leaf decomposition is extremely rapid, resulting in very fast nutrient cycling on the forest floor. If non-endemic leaf species are placed in the peat swamp forests, they break down quite quickly, but even after one year submerged in the swamp, endemic species remain virtually unchanged (Yule and Gomez 2008). The only nutrients available for the trees are thus the ones that leach from the leaves when they fall, and these nutrients are rapidly absorbed by the thick root mat. It was previously assumed that the low pH and anaerobic conditions of the tropical peat swamps meant that bacteria and fungi could not survive, but recent studies have shown diverse and abundant communities (albeit not nearly as diverse as dry land tropical rainforests, or freshwater swamps) (Voglmayr and Yule 2006; Jackson, Liew and Yule 2008).

Fauna

These forests are home to wildlife including gibbons, orangutans, and crocodiles. In particular the riverbanks of the swamps are important habitats for the crab-eating macaque (Macaca fascicularis) and the silvery lutung (Presbytis cristata) and are the main habitat of Borneo's unique and endangered proboscis monkey (Nasalis larvatus) which can swim well in the rivers, and the Borneo roundleaf bat (Hipposideros doriae). There are two birds endemic to the peat forests, the Javan white-eye (Zosterops flavus) and the hook-billed bulbul (Setornis criniger) while more than 200 species of birds have been recorded in Tanjung Puting National Park in Kalimantan. Rivers of the peat swamps are home to the rare arowana fish (Scleropages formosus), otters, waterbirds, false gharials and crocodiles. Another small species of fish are the Parosphromenus which are also extremely endangered. The parosphromenus species are small fish of extreme beauty.

Preservation

Attempts at preservation have been minimal in comparison to recent devastation while commercial logging of peat swamp forest in Sarawak is ongoing and planned to intensify in Brunei. One plan by the environmental NGO Borneo Orangutan Survival is to preserve the peat swamp forest of Mawas using a combination of carbon finance and debt-for-nature-swap. Peatland conservation and rehabilitation are more efficient undertakings than reducing deforestation (in terms of claiming carbon credits through REDD initiatives) due to the much larger reduced emissions achievable per unit area and the much lower opportunity costs involved. [12] About 6% of the original peat-forest area is contained within protected areas, the largest of which are Tanjung Puting and Sabangau National Parks.

See also

Related Research Articles

<span class="mw-page-title-main">Peat</span> Accumulation of partially decayed vegetation

Peat, also known as turf, is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem covers 3.7 million square kilometres (1.4 million square miles) and is the most efficient carbon sink on the planet, because peatland plants capture carbon dioxide (CO2) naturally released from the peat, maintaining an equilibrium. In natural peatlands, the "annual rate of biomass production is greater than the rate of decomposition", but it takes "thousands of years for peatlands to develop the deposits of 1.5 to 2.3 m [4.9 to 7.5 ft], which is the average depth of the boreal [northern] peatlands", which store around 415 gigatonnes (Gt) of carbon (about 46 times 2019 global CO2 emissions). Globally, peat stores up to 550 Gt of carbon, 42% of all soil carbon, which exceeds the carbon stored in all other vegetation types, including the world's forests, although it covers just 3% of the land's surface. Sphagnum moss, also called peat moss, is one of the most common components in peat, although many other plants can contribute. The biological features of sphagnum mosses act to create a habitat aiding peat formation, a phenomenon termed 'habitat manipulation'. Soils consisting primarily of peat are known as histosols. Peat forms in wetland conditions, where flooding or stagnant water obstructs the flow of oxygen from the atmosphere, slowing the rate of decomposition. Peat properties such as organic matter content and saturated hydraulic conductivity can exhibit high spatial heterogeneity.

<span class="mw-page-title-main">Peat swamp forest</span> Tropical moist forests where waterlogged soil prevents dead leaves and wood from fully decomposing

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<span class="mw-page-title-main">1997 Southeast Asian haze</span> Haze over the Southeast Asia region in mid-1997

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<span class="mw-page-title-main">Storm's stork</span> Species of bird

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<span class="mw-page-title-main">Tropical peat</span>

Tropical peat is a type of histosol that is found in tropical latitudes, including South East Asia, Africa, and Central and South America. Tropical peat mostly consists of dead organic matter from trees instead of spaghnum which are commonly found in temperate peat. This soils usually contain high organic matter content, exceeding 75% with dry low bulk density around 0.2 mg/m3 (0.0 gr/cu ft).

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The Kahayan river, or Great Dayak River, is the second largest river after Barito River in Central Kalimantan, a province of Indonesia in Kalimantan – the Indonesian part of the island of Borneo. With a total length of 658 km (409 mi) and with a drainage basin of 15,500 km2 (6,000 sq mi) in South Kalimantan, Indonesia. Mean annual discharge 1,178 m3/s (41,600 cu ft/s). The provincial capital Palangkaraya lies on the river. The main inhabitants are Dayaks, who practice slash-and-burn rice cultivation and pan for gold on the upper reaches. The lower Kayahan flows through a rich and unusual environment of peat swamp forests, which has been severely degraded by an unsuccessful program to convert a large part of the area into rice paddies, compounded by legal and illegal forestry.

<span class="mw-page-title-main">Mega Rice Project</span> Abandoned agricultural project in Indonesian Borneo

The Mega Rice Project was initiated in 1996 in the southern sections of Kalimantan, the Indonesian section of Borneo. The goal was to turn one million hectares of unproductive and sparsely populated peat swamp forest into rice paddies in an effort to alleviate Indonesia's growing food shortage. The government made a large investment in constructing irrigation canals and removing trees. The project did not succeed, and was eventually abandoned after causing considerable damage to the environment.

<span class="mw-page-title-main">Sabangau National Park</span> National park in Indonesia

Sabangau National Park is a national park in Central Kalimantan, a province of Indonesia in Kalimantan, the Indonesian part of the island of Borneo established in 2004. Between 1980 and 1995 the site was a massive logging concessions area. After 1995, the park became a site for illegal logging, which resulted in up to 85 percent of the 568,700-hectare total park area being destroyed. By 2012, less than 1 percent of the park's total area has been reforested and several centuries is needed to restore it to its pre-logged state.

<span class="mw-page-title-main">1997 Indonesian forest fires</span>

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<span class="mw-page-title-main">Borneo lowland rain forests</span> Ecoregion in Borneo

The Borneo lowland rain forests is an ecoregion, within the tropical and subtropical moist broadleaf forests biome, of the large island of Borneo in Southeast Asia. It supports approximately 15,000 plant species, 380 bird species and several mammal species. The Borneo lowland rain forests is diminishing due to logging, hunting and conversion to commercial land use.

<span class="mw-page-title-main">Environment of Malaysia</span> Megadiverse ecology with rainforests and ocean

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<span class="mw-page-title-main">Rimba Raya Biodiversity Reserve</span>

The Rimba Raya Biodiversity Reserve, nearly the size of Singapore, consists of 64,000 hectares of bio-diverse tropical peat swamp forest that contain as much as 1,000 plant and animal species per hectare and is one of the most highly endangered ecosystems on the planet. The project area and ongoing initiatives focus on environmental conservation, community outreach, and climate control. Rimba Raya is home to one of the few remaining relic populations of wild orangutans and is the largest privately funded orangutan reserve in the world. The area is also one of the world’s largest repositories of carbon. Rimba Raya is the world’s largest REDD+ project -Reduced Emissions from (Avoided) Deforestation and Degradation (REDD). The project developer, InfiniteEARTH, is an industry pioneer, delivering the world’s first REDD methodology in 2009.

<span class="mw-page-title-main">Mire</span> Wetland terrain without forest cover, dominated by living, peat-forming plants

A mire, peatland, or quagmire is a wetland area dominated by living peat-forming plants. Mires arise because of incomplete decomposition of organic matter, usually litter from vegetation, due to water-logging and subsequent anoxia. All types of mires share the common characteristic of being saturated with water, at least seasonally with actively forming peat, while having their own ecosystem. Like coral reefs, mires are unusual landforms that derive mostly from biological rather than physical processes, and can take on characteristic shapes and surface patterning.

Paludiculture is wet agriculture and forestry on peatlands. Paludiculture combines the reduction of greenhouse gas emissions from drained peatlands through rewetting with continued land use and biomass production under wet conditions. “Paludi” comes from the Latin “palus” meaning “swamp, morass” and "paludiculture" as a concept was developed at Greifswald University. Paludiculture is a sustainable alternative to drainage-based agriculture, intended to maintain carbon storage in peatlands. This differentiates paludiculture from agriculture like rice paddies, which involve draining, and therefore degrading wetlands.

<span class="mw-page-title-main">2019 Southeast Asian haze</span> Haze over the Southeast Asia region in mid-2019

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References

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  4. Pearce, Fred (12 August 2002), "Borneo fires may intensify 'Asian brown haze'", New Scientist, retrieved 11 April 2010 The smog from fires killed "as many as a million people a year from respiratory diseases" according to UNEP director Klaus Toepfer.
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Sources