Tonlé Sap Lake is located in the northwest of the lower Mekong plain, formed by the collision and collapse of theIndian Plate and theEurasian Plate.[7] The lower Mekong plain used to be a bay, and the sea level rose rapidly at the end of the lastglacial period. About 4.5 metres (15 ft) high, cores from this period found near Angkor contain tidal deposits, as well as salt marshes andmangrove swamp deposits,[8] deposited in caves about 7,900-7,300 years ago. The sediments of Lake Sap also show signs of marine influence.[9] The current river morphology of the Mekong Delta was developed over the past 6,000 years,[10] while the remaining waters in the northwest corner of the lower Mekong plain formed the Tonlé Sap.[11]
The Tonlé Sapdrainage basin is bordered to the southwest by theCardamom Mountains, with heights of more than 1,700 metres (5,600 ft), and to the north are the Piandan Mountains with an average height of 500 metres (1,600 ft). The basin covers an area of 86,000 square kilometres (33,000 sq mi). The 120 kilometres (75 mi)-longTonlé Sap River connects the Tonlé Sap Lake with the Mekong River and contributes 9% of the flow of the Mekong River.[6][12] The size and water volume of the lake varies greatly throughout the year, with a minimum area of about 2,500–3,000 square kilometres (970–1,160 sq mi) and a volume of about 1 cubic kilometre (0.24 cu mi) in the dry season,[13] and the water body expands in the rainy season, increasing the depth to 9–14 metres (30–46 ft).[14] The maximum area is 16,000 square kilometres (6,200 sq mi), and the volume is about 80 cubic kilometres (19 cu mi).[13]
About 34% of the water in the Tonlé Sap comes from the rivers that enter the lake, about 53.5% from the Mekong River, and 12.5% from precipitation.[6] May to October is the rainy season in the lower Mekong plain, and November to March is the dry season. The annual rainfall is 1,000 to 4,000 millimetres (39 to 157 in). Almost all the precipitation is in the rainy season.[15] At the end of the dry season, the Tonlé Sap Lake has a typical depth of 1 metre (3.3 ft). As themonsoon rain begins, thewater level of the river begins to rise, eventually reversing the flow of the river. The water level of the Tonlé Sap increases by about 10 metres (33 ft), the flow of the Mekong gradually decreases at the end of the rainy season, and the flow of the Tonlé Sap then reverses and begins to replenish the flow of the Mekong.[3]
The extreme hydrodynamic complexity of the Tonlé Sap Lake, both in time and space, makes it impossible to measure specific flow, and water level rather than velocity and volume determines the movement of water as it shapes the landscape.[13] 72% of the modern sediments deposited in the Tonlé Sap come from the Mekong River, while only 28% come from the catchments upstream of the lake.[11] Sediment-bound phosphorus acts as the basis of the food chain through phytoplankton, and internal nutrient cycling plays a crucial role in the productivity of thefloodplain and, therefore, the long-term sustainability of the lake's entire ecosystem.[16]
The land cover of the Tonlé Sap Basin is 55% forest and 45% agricultural land.[6] The lake is surrounded by freshwater mangroves known as "flood forests",[17] accounting for 3% of the basin area,[6] and the floodplain is surrounded by low hills and covered with evergreen or deciduous seasonal tropical plants. The forest is dominated byDipterocarpaceae,Leguminosae, Lacelandaceae, and in some places Pinaceae, Rohan pineaceae or bamboo. Farther from the lake, the forest gradually turns into a thicket, and finally into a meadow.[17][18] In areas with higher quality soils or higher altitudes, deciduous mixed forests and semi-evergreen forests occur.[19][20] This diversity of vegetation types underlies the species diversity of the Tonle Sap ecosystem, with interlocking forests, grasslands and swamps providing refuge for local wildlife.[20]
The lake is home to at least 149 species of fish, 11 of which are globally endangered, and the lake area is also home to 6 near-threatened species, including spotted-billed, great bald, Bengal, black-bellied, andGrey-headed fish eagle and Far Eastern reed, in addition to supporting reptile populations including the endangeredSiamese crocodile and numerous freshwater snakes, and although much of the Lake District has been turned into farmland, 200 species of higher plants are still recorded.[21] TheMekong giant catfish, which lives in the Tonlé Sap Lake, is one of the largest freshwater fish in the world. A fisherman caught a Mekong giant catfish weighing nearly 648 pounds in May 2004, but its population has been declining since the mid-1970s. It is currently illegal for fishermen to catch and retain Mekong giant catfish, and only a few are used for scientific research.[22]
As a natural flood reservoir for the entire Mekong River system, Tonlé Sap Lake regulates floods in the lower reaches of Phnom Penh during the rainy season, and is also an important supplement to the dry season flow of theMekong Delta.[23] In 1997,UNESCO designated the Tonle Sap as a biosphere reserve, but scientists have been concerned that high dams built in southern China and Laos will affect the strength and flow of countercurrents into the Tonlé Sap, reducing the number of fish in the lake. Tonle Sap habitat for nesting, breeding, spawning, and foraging in the floodplain, which will adversely affect fish productivity and overall biodiversity in the Tonle Sap.[24][25]
Forest loss hotspots are located in low floodplain areas where protected areas are located, significant farmland expansion is mainly in the intersection between the lower and upper floodplains, population growth, fuelwood gathering and logging are the main causes of forest loss, intensification of agricultural activities and upstream hydropower development reduces buffers to natural habitats and increases the risk of forest loss.[26] By the 2030s, hydropower development may lead to large-scale changes in habitat, with the area of coastal forests likely to decrease by 82%, while the area of rain-fed habitats may increase by 10–13%.[27] In July 2020, under the influence of the El Niño phenomenon and the impoundment of dams in the tributaries of the Mekong River, the water level of the Tonle Sap Lake hit a record low for the same period in the past 60 years.[28]
The Tonlé Sap Lake District has always been a vital fishing and agricultural production area for Cambodia, and it has largely maintainedAngkor, the largest pre-industrial settlement complex in history.[29] While many fish left lakes and ponds to spawn in flooded forests at the onset of floods, the inflow of Mekong floods brought large numbers of fry, which found shelter and food in flooded forests and floodplains.[17]
The approximately 1.2 million people who live in the Tonlé Sap Lake area, which accounts for about 60% of Cambodia's annual freshwater catch of over 400,000 tons, account for 60% of the country's population's protein intake.[30][31][32] Most fish are eaten fresh, and savory and fermented fish pastePrahoc is usually marinated from the least popular fish or leftover fish that cannot be sold fresh.[17] For more than a century, the most productive lake areas have been privatized through a government-lease system of fishing grounds, providing more than $2 million in tax revenue annually.[30]
Floating school on Tonlé Sap
Since Buddhism is against killing, fishermen tend to limit their catch to what they can feed their families. They do not kill the fish with their own hands but wait for the fish to die naturally after they leave the water. At the end of the rice season, people restore canoes that have been in use for hundreds of years or build new canoes when they can't be repaired in temples along the river, in preparation for the boating competition of the water festival. After two days of racing all the canoes come together to celebrate theNaga, the water serpent, who supposedly spit out the lake into the sea at the end of the rainy season,[33] while bringing fish into the Mekong through the Tonlé Sap River.[17]
The area is home to manyCambodians of Vietnamese origin who live in floating villages on boats by the lake.[34] Most of the fishermen of Tonlé Sap Lake are of Vietnamese origin. They have lived in Cambodia for a long time and are the main suppliers of the country's fishery market. They had to flee to Vietnam during theKhmer Rouge era from 1975 to 1979. After thedownfall of the regime, they returned and continued to fish in the Tonle Sap.[35]
^Tjia, H. D. (28 April 2014). "Wrench-Slip Reversals and Structural Inversions: Cenozoic Slide-Rule Tectonics in Sundaland".Indonesian Journal on Geoscience.1 (1). Institute for Environment and Development University Kebangsaan Malaysia:35–52.doi:10.17014/ijog.v1i1.174 (inactive 12 July 2025).{{cite journal}}: CS1 maint: DOI inactive as of July 2025 (link)
^Chadwick, M T; Juntopas, M; Sithirith, M (2008).Sustaining Tonle Sap: An Assessment of Development Challenges Facing the Great Lake. Bangkok: The Sustainable Mekong Research Network.ISBN9789186125066.
Kuenzer, C. (2013): "Field Note: Threatening Tonle Sap: Challenges for Southeast-Asia’s largest Freshwater Lake." In:Pacific Geographies 40, pp. 29–31.
