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Peat swamp forest

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53: 701: 689: 611: 677: 564: 33: 756:) 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. 2912: 293: 2901: 922: 767:, 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. 648:
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.
590:. 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. 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. 647:
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
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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
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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. Peat
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Crezee, Bart; Dargie, Greta C.; Ewango, Corneille E. N.; Mitchard, Edward T. A.; Emba B., Ovide; Kanyama T., Joseph; Bola, Pierre; Ndjango, Jean-Bosco N.; Girkin, Nicholas T.; Bocko, Yannick E.; Ifo, Suspense A.; Hubau, Wannes; Seidensticker, Dirk; Batumike, Rodrigue; Imani, Gérard (21 July 2022).
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Rieley JO, Ahmad-Shah AA Brady MA (1996) The extent and nature of tropical peat swamps. In: Maltby E, Immirzi CP, Safford RJ (eds) Tropical lowland peatlands of Southeast Asia, proceedings of a workshop on integrated planning and management of tropical lowland peatlands held at Cisarua, Indonesia,
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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
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by water plants, then transform into waterlogged swamp with grasses or shrubs, and eventually formed a forest that continues to grow and accumulate. Peat located on the fringing areas of domes in between domes might form through lateral expansion. This peat accumulation often forms a convex shape
670:(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. 597:
with characteristics of high organic material content (70–99%). 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
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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
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Page, S. E.; Wűst, R. A. J.; Weiss, D.; Rieley, J. O.; Shotyk, W.; Limin, S. H. (2004). "A record of Late Pleistocene and Holocene carbon accumulation and climate change from an equatorial peat bog (Kalimantan, Indonesia): implications for past, present and future carbon dynamics".
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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. A similar pattern is observed in cores from Sentarum,
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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. At the beginning of its formation, peat is largely topogenous or minerotrophic, receiving high nutrient input from rivers or
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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 NGO
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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
700: 486:, exclusively obtaining water from the precipitation 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. 770:
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 of
376:; they are among the largest near-surface reserves of terrestrial organic carbon. Tropical peat swamp forests, which have ecological importance, are one of the most threatened, yet least studied and most poorly understood biotypes. 820:, 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. 391:(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 as 571:
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 by
446:). Peat in Indonesia is distributed over three islands, Sumatra (8.3 million ha), Kalimantan (6.3 million ha) and Papua (4.6 million ha). 36% of the world's tropical peat occurs in Africa's central Congo Basin. 1209:
Page SE, Rieley JO, Wüst R (2006) Lowland tropical peatlands of Southeast Asia In: Martini IP, Martínez Cortizas A, Chesworth W (eds) Peatlands: Evolution and Records of Environmental and Climate Changes. Elsevier BV pp
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Dommain, R.; Couwenberg, J.; Joosten, H. (2011). "Development and carbon sequestration of tropical peat domes in South-east Asia: links to post-glacial sea-level changes and Holocene climate variability".
530:, 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. 547:, where the peat shows slower growth around 28-16000 BP, 13-3000 BP and on 5-3000 BP. While the slower growth from 28 to 16000 BP and 5-3000 BP is explained by a drier climate during this period due to 667: 1922:
Page, Susan E.; Siegert, Florian; Rieley, John O.; Boehm, Hans-Dieter V.; Jaya, Adi; Limin, Suwido (2002). "The amount of carbon released from peat and forest fires in Indonesia during 1997".
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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 the
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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 and
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Anshari, G.; Peter Kershaw, A.; Van Der Kaars, S.; Jacobsen, G. (2004). "Environmental change and peatland forest dynamics in the Lake Sentarum area, West Kalimantan, Indonesia".
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Partin, J. W.; Cobb, K. M.; Adkins, J. F.; Clark, B. and Fernandez, D. P. (2007). "Millennial-scale trends in west Pacific warm pool hydrology since the Last Glacial Maximum".
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Lewis, Simon L.; Ifo, Suspense A.; Bocko, Yannick E.; Page, Susan E.; Mitchard, Edward T. A.; Miles, Lera; Rayden, Tim J.; Lawson, Ian T.; Dargie, Greta C. (16 January 2018).
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Cameron, C. C.; Esterle, J. S.; Palmer, C. A. (1989). "The geology, botany and chemistry of selected peat-forming environments from temperate and tropical latitudes".
339: 372:; because the decomposition of the organic matter is slower than its production rate, the surplus accumulates as peat. Their stability has important implications for 1463:
Anshari, G. (2001). "A Late Pleistocene and Holocene pollen and charcoal record from peat swamp forest, Lake Sentarum Wildlife Reserve, West Kalimantan, Indonesia".
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concentration detected since records began in 1957. Additionally, the 2002–03 fires released between 200 million to 1 billion tons of carbon into the atmosphere.
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Wösten, J.H.M.; Clymans, E.; Page, S.E.; Rieley, J.O.; Limin, S.H. (2008). "Peat–water interrelationships in a tropical peatland ecosystem in Southeast Asia".
498:, about 8000 years ago. Inland peat formed much earlier during the Late Pleistocene, more than 26000 BP. Coastal peat formation is highly affected by the 482:. 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 becoming 1812:
Gagan, M. K.; Hendy, E. J.; Haberle, S. G.; Hantoro, W. S. (2004). "Post-glacial evolution of the Indo-Pacific Warm Pool and El Niño-Southern oscillation".
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Tropical peat ecosystem are found in three regions: Central America, Africa and South East Asia. About 62% of the world's tropical peat lands occur in the
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mosses, grasses, sedges and shrubs). The spongy, unstable, waterlogged, anaerobic beds of peat can be up to 20 m (66 ft) deep with low
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Indonesia is currently the world's third largest carbon emitter, to a large extent due to the destruction of its ancient peat swamp forests.
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Tropical peat swamp forests are home to thousands of animals and plants, including many rare and critically endangered species such as the
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Borneo lowlands to the north-west and south-east shrouded with thick, grey smoke from dozens of fires in this satellite image from 2009
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been reduced through deforestation, drainage, and conversion to agricultural lands and other activities. Their current status as
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where waterlogged soil prevents dead leaves and wood from fully decomposing. Over time, this creates a thick layer of acidic
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atmosphere, exacerbating human-made climate change. Estimation of carbon content of tropical peat ranges from 50 
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Hirano, Takashi. (29 November 2006). Carbon dioxide balance of a tropical peat swamp forest in Kalimantan, Indonesia.
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Couwenberg, J.; Dommain, R.; Joosten, H. (2009). "Greenhouse gas fluxes from tropical peatlands in south-east Asia".
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Yule, Catherine M. (22 June 2008). Leaf litter decomposition in a tropical peat swamp forest in Peninsular Malaysia.
2775: 582:(pH 2.9 – 4) and low nutrients, and the forest floor is seasonally flooded. The water is stained dark brown by the 196: 962: 956: 829: 722: 718: 640: 276: 264: 213: 165: 160: 155: 145: 140: 135: 117: 112: 82: 62: 2754: 851: 1150: 2465: 1175: 977: 800: 191: 2800: 2677: 2571: 2098: 1632: 812: 764: 738: 733:. About 6% of the original peat-forest area is contained within protected areas, the largest of which are 535: 1843:
Yule, C. M. (2010). "Loss of biodiversity and ecosystem functioning in Indo-Malayan peat swamp forests".
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Satellite image of the island of Borneo on 19 August 2002, showing smoke from burning peat swamp forests
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Smith, D. E.; Harrison, S.; Firth, C. R.; Jordan, J. T. (2011). "The early Holocene sea level rise".
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Peat swamp forests are typically surrounded by lowland rain forests on better-drained soils, and by
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Tropical moist forests where waterlogged soil prevents dead leaves and wood from fully decomposing
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Sorensen, Kim W. (September 1993). Indonesian peat swamp forests and their role as a carbon sink.
1895: 1860: 1780: 1729: 1686: 1407: 1399: 1090: 368:—much more than forests on mineral soil (i.e. non-peatland) contain. Peat formation is a natural 32: 2915: 2825: 2732: 2541: 2346: 2321: 2091: 2057: 1955: 1947: 1772: 1314: 1262: 1244: 1131: 1082: 636: 494:
Inland and coastal peat differ greatly in their age, where coastal peat formed during the mid
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is tectonically stable, the sea level change in this area is only affected by the eustatic
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Woodroffe, S. A.; Horton, B.P. (2005). "Holocene sea-level changes in the Indo-Pacific".
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and unsustainable palm oil expansion in Indonesia's peatlands, organizations, such as
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with strong accumulation around 8-4000 BP when El Nino is less intense. Because the
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Peat forest contains high amount of carbon due to its soil nature, categorized as
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Philosophical Transactions of the Royal Society of London B: Biological Sciences
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Envisat focuses on carbon-rich peat swamp forest fires (European Space Agency)
2052: 1856: 1126: 917: 883: 772: 639:(MRP), the government of Indonesia has drained over 1 million hectares of the 552: 463: 459: 2061: 1951: 1318: 1248: 1135: 1086: 2657: 2631: 2366: 2180: 2155: 2135: 1109: 837: 760: 745: 599: 507: 467: 419: 399: 1959: 1776: 1266: 1240: 1503:
Yu, Z.; Loisel, J.; Brosseau, D. P.; Beilman, D. W.; Hunt, S.e J. (2010).
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Page, Susan E.; Rieley, John O.; Banks, Christopher J. (1 February 2011).
17: 2845: 2840: 2830: 2652: 2604: 2599: 2582: 2440: 2420: 2385: 2301: 2264: 2259: 1529: 1504: 1025:"The structure and development of the peat swamps of Sarawak and Burunei" 1024: 899: 869: 865: 841: 749: 594: 574: 495: 443: 423: 384: 354: 350: 1943: 1768: 1225:"Interdependence of peat and vegetation in a tropical peat swamp forest" 1223:
Page, S. E.; Rieley, J. O.; Shotyk, Ø W.; Weiss, D. (29 November 1999).
775:'s peat swamp forests in light of recent and rapid habitat degradation. 2880: 2860: 2425: 2390: 2212: 2114: 1403: 1309: 903: 515: 435: 2614: 2405: 2395: 2291: 1053:"Global and regional importance of the tropical peatland carbon pool" 833: 615: 583: 519: 431: 58: 1725: 1682: 1395: 2455: 2410: 2400: 2380: 2331: 2296: 2271: 2244: 2140: 1108:
Murdiyarso, Daniel; Lilleskov, Erik; Kolka, Randy (1 April 2019).
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Satellite photograph of the haze above Borneo on 5 October 2006
346:. Large areas of these forests are being logged at high rates. 2249: 2160: 935: 816:) were barely decomposed by bacteria and fungi, the leaves of 1992:"RI's peat forests can play important role in climate change" 2033:"Congo Basin peatlands: threats and conservation priorities" 1980:
Mathai, J. (5 October 2009). Seeing REDD over deforestation.
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reducing emissions from deforestation and forest degradation
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that leach from the fallen leaves and peat – hence the name
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have greatly increased in South East Asia. In addition,
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Pages displaying short descriptions of redirect targets
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Mitigation and Adaptation Strategies for Global Change
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Mitigation and Adaptation Strategies for Global Change
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1558:2011QSRv...30.1846S 1521:2010GeoRL..3713402Y 1477:2001PPP...171..213A 1442:2008Caten..73..212W 1357:1989IJCG...12..105C 1235:(1391): 1885–1897. 1069:2011GCBio..17..798P 807:Pandanus atrocarpus 624:carbon sequestering 366:soil organic matter 360:They are a kind of 151:2016 Malaysian haze 108:2005 Malaysian haze 2750:Salt marsh die-off 2668:Salt marsh dieback 2577:List of fen plants 2416:Palustrine wetland 2317:Intertidal wetland 2312:Interdunal wetland 995:The Burning Season 795:Macaranga pruinosa 619: 569: 336:Peat swamp forests 38: 2924: 2923: 2826:Aquatic ecosystem 2814: 2813: 2733:Ramsar Convention 2560: 2559: 2542:Converted wetland 2484:Peat swamp forest 2347:Inland salt marsh 1588:(7–8): 999–1010. 1287:Nature Geoscience 971: – soil type 637:Mega Rice Project 588:blackwater swamps 430:, and pockets in 416:Indomalayan realm 333: 332: 209:Peat swamp forest 204:Mega Rice Project 16:(Redirected from 2964: 2914: 2913: 2904: 2903: 2902: 2886:Will-o'-the-wisp 2819:Related articles 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311: 300: 295: 294: 184:Chemical equator 55: 40: 21: 2972: 2971: 2967: 2966: 2965: 2963: 2962: 2961: 2927: 2926: 2925: 2920: 2900: 2898: 2890: 2810: 2781:Ducks Unlimited 2759: 2718:Clean Water Act 2700: 2678:Classifications 2672: 2641: 2588: 2556: 2520: 2471:Mangrove forest 2117: 2112: 2075: 2070: 2069: 2035: 2030: 2029: 2025: 2020: 2016: 2011: 2007: 1989: 1988: 1984: 1979: 1975: 1930:(6911): 61–65. 1921: 1920: 1916: 1911: 1907: 1877: 1876: 1872: 1842: 1841: 1837: 1811: 1810: 1806: 1789: 1755:(7161): 452–5. 1746: 1745: 1741: 1726:10.1002/jqs.879 1703: 1702: 1698: 1683:10.1002/jqs.884 1659: 1658: 1654: 1638:10.1.1.693.8047 1614: 1613: 1609: 1578: 1577: 1573: 1543: 1542: 1538: 1502: 1501: 1492: 1462: 1461: 1457: 1427: 1426: 1419: 1396:10.2307/1552080 1377: 1376: 1372: 1342: 1341: 1326: 1279: 1278: 1274: 1222: 1221: 1214: 1208: 1204: 1198: 1194: 1184: 1182: 1174: 1173: 1169: 1159: 1157: 1148: 1147: 1143: 1107: 1106: 1102: 1050: 1049: 1040: 1022: 1021: 1010: 1005: 972: 951: 928:Wetlands portal 926: 921: 919: 916: 880:Sylhet District 826: 781: 748:continue to be 714: 707: 704: 695: 692: 683: 680: 659: 645:illegal logging 633: 608: 561: 545:West Kalimantan 512:Karimata Strait 492: 490:South East Asia 452: 412: 329: 290: 233: 171: 170: 131: 123: 122: 103: 95: 94: 78: 65: 28: 23: 22: 15: 12: 11: 5: 2970: 2968: 2960: 2959: 2954: 2949: 2944: 2939: 2929: 2928: 2922: 2921: 2919: 2918: 2908: 2895: 2892: 2891: 2889: 2888: 2883: 2878: 2873: 2868: 2863: 2858: 2856:Drainage basin 2853: 2848: 2843: 2838: 2833: 2828: 2822: 2820: 2816: 2815: 2812: 2811: 2809: 2808: 2803: 2798: 2793: 2788: 2783: 2778: 2773: 2767: 2765: 2761: 2760: 2758: 2757: 2752: 2747: 2746: 2745: 2735: 2730: 2725: 2720: 2714: 2708: 2702: 2701: 2699: 2698: 2693: 2688: 2682: 2680: 2674: 2673: 2671: 2670: 2665: 2663:Paludification 2660: 2655: 2649: 2647: 2643: 2642: 2640: 2639: 2634: 2629: 2624: 2623: 2622: 2617: 2615:Sapric or muck 2612: 2602: 2596: 2594: 2593:Soil mechanics 2590: 2589: 2587: 2586: 2579: 2574: 2568: 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2527: 2523: 2517: 2514: 2512: 2509: 2507: 2504: 2502: 2501:Várzea forest 2499: 2497: 2494: 2490: 2487: 2485: 2482: 2480: 2478: 2474: 2472: 2469: 2467: 2464: 2462: 2459: 2458: 2457: 2454: 2452: 2449: 2447: 2444: 2442: 2439: 2437: 2434: 2432: 2429: 2427: 2424: 2422: 2419: 2417: 2414: 2412: 2409: 2407: 2404: 2402: 2399: 2397: 2394: 2392: 2389: 2387: 2384: 2382: 2379: 2377: 2374: 2368: 2365: 2363: 2360: 2359: 2358: 2355: 2353: 2350: 2348: 2345: 2343: 2340: 2338: 2335: 2334: 2333: 2330: 2328: 2325: 2323: 2320: 2318: 2315: 2313: 2310: 2308: 2305: 2303: 2300: 2298: 2295: 2293: 2290: 2288: 2285: 2283: 2280: 2278: 2275: 2273: 2270: 2266: 2263: 2261: 2258: 2256: 2253: 2252: 2251: 2248: 2246: 2243: 2241: 2238: 2236: 2233: 2231: 2228: 2224: 2221: 2220: 2219: 2216: 2214: 2211: 2207: 2204: 2202: 2199: 2197: 2194: 2192: 2191:Polygonal bog 2189: 2187: 2184: 2182: 2179: 2177: 2174: 2172: 2169: 2167: 2164: 2163: 2162: 2159: 2157: 2154: 2152: 2149: 2147: 2144: 2142: 2139: 2137: 2134: 2133: 2131: 2127: 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2637:Ombrotrophic 2581: 2552:Water-meadow 2483: 2476: 2287:Grass valley 2277:Flood-meadow 2240:Cypress dome 2171:Cataract bog 2146:Beach meadow 2043: 2039: 2026: 2017: 2008: 1995: 1985: 1976: 1927: 1923: 1917: 1908: 1883: 1879: 1873: 1848: 1844: 1838: 1813: 1807: 1793:cite journal 1752: 1748: 1742: 1709: 1705: 1699: 1666: 1662: 1655: 1623:(1): 29–43. 1620: 1616: 1610: 1585: 1581: 1574: 1549: 1545: 1539: 1512: 1508: 1468: 1464: 1458: 1433: 1429: 1387: 1383: 1373: 1348: 1344: 1290: 1286: 1275: 1232: 1228: 1205: 1195: 1183:. 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Index

Peat swamp

Southeast Asian haze

Borneo
2019
1997 Southeast Asian haze
1997 Indonesian forest fires
2005 Malaysian haze
2006 Southeast Asian haze
2009 Southeast Asian haze
2010 Southeast Asian haze
2013 Southeast Asian haze
2015 Southeast Asian haze
2016 Malaysian haze
2016 Southeast Asian haze
2017 Southeast Asian haze
2019 Southeast Asian haze
Chemical equator
in Borneo
in Indonesia
Mega Rice Project
Peat swamp forest
Borneo
ASEAN Agreement on Transboundary
Haze Pollution

Operation Haze
Transboundary Haze Pollution Act 2014
People's Movement to Stop Haze
Air pollution in Malaysia
API

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