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The Sri Lanka Montane Rain Forests [IM0155] represents the montane and submontane moist forests above 1,000 m in the central massif and in the Knuckles Mountain Range to the northeast. Sri Lanka first separated from the Deccan Peninsula during the late Miocene, but geologically it has Gondwanaland origins. The biogeographic patterns indicate that the wet forests in the southwestern quarter became isolated from the nearest other wet forests in the mainland soon after the first separation when climatic changes created drier, warmer conditions throughout most of the lowland areas (Deraniyagala 1992). During subsequent Pleistocene-period land-bridge connections, the intervening drier habitat prevented the exchange of wet forest-adapted species with the wet forests in India. Therefore, the species in the southwestern quarter evolved and speciated in isolation, giving rise to the high levels of endemism that are evident today (Senanayake 1993; Wikramanayake 1990). The post-Miocene uplift that created three peneplains, or steep plains of erosion (Deraniyagala 1958), have also served as biogeographic barriers, isolating taxonomic groups (Senanayake 1993; Wikramanayake 1990). This is best exemplified in the distribution of the freshwater fish fauna, where the lowland streams have the highest species richness, the second peneplain fewer, and the upper peneplain streams support a limited fish fauna (Wikramanayake 1990). Floral surveys also show that plant diversity is greater in the lowland forests but that the montane forests support greater numbers of endemic plants (Singhakumara 1995). The higher peaks of the central massif attain heights of more than 2,500 m, but the average height is about 1,800 m. The isolated Knuckles Range to the northwest of the central massif rises to more than 1,800 m, but the main range is about 1,500 m. All of Sri Lanka's major rivers originate in the central mountains and radiate outward. The predominant soil type is red-yellow podzolic soils (Survey Department 1988). There is a general trend of a 0.5(C decrease in air temperature for every 100-m rise in elevation (Ashton et al. 1997); therefore, the climate is cooler than in the lowlands. Ground frost is not uncommon in the higher elevations during the nights from December to February. Many of the high peaks are also enveloped in mist and fog, creating cloud forests. The ecoregion receives 2,500-5,000 mm of annual rainfall. Most of the rainfall is from the May to September southwestern monsoon, which expends its moisture on the western, windward side. The northeastern monsoon, which sweeps in from the northeastern coast and ascends the gentler eastern slopes, brings additional rainfall to the ecoregion from December to March. The vegetation is influenced primarily by climate (de Rosayro 1950) and ranges from Dipterocarpus-dominated montane moist forests to montane savanna and cloud forests with Rhododendron species. The submontane forests in the central massif are dominated by a Shorea-Calophyllum-Syzygium community with a canopy of Shorea gardneri, S. trapezifolia, Palaquium spp., Homalium zelanicum, Calophyllum calaba, C. tomentosum, C. pulcherrimum, Syzygium spp., Cullenia spp., Myristica dactyloides, Cryptocarya wightiana, and Neolitsea involucrata (Ashton and Gunatilleke 1987; Singhakumara 1995). The forests above 1,500 m are composed of twisted, stunted Syzygium-Gordonia-Michelia-Elaeocarpus formations, draped in a rich epiphytic community of orchids, mosses, and filmy ferns, and a Strobilanthes-dominated understory (Singhakumara 1995). Other prominent genera include Cinnamomum, Litsea, Neolitsea, Symplocus, Semecarpus, Carallia, Garcinia, and Mastixia. The montane forests of the Peak Wilderness area have forests that are locally dominated by the endemic Dipterocarpaceae genus Stemnoporus, possibly representing the only area of a dipterocarp-dominated montane forest (Singhakumara 1995), but in general the montane forests are dominated by Lauraceae, Myrtaceae, Clusiaceae, and Symplocaceae. Rhododendron species occur at the highest elevations-where cloud forests prevail-and in the transition zones with the wet montane grasslands, locally known as wet pathanas. These grasslands are thought to be fire-maintained and support a rich herb community with both temperate and tropical elements. Several animal species have also adapted their life history and behavior (e.g., nesting patterns) to these fire regimes. Not too long ago, Asian elephants (Elephas maximus) roamed these savannas (Phillips 1980), although they have now become locally extinct. The flora of the detached Knuckles Range is different from the central massif flora and is characterized by a Myristica-Cullenia-Aglaia-Litsea community with subtropical affinities and a tropical Callophyllum zone (Gunatilleke and Gunatilleke 1990).
The montane forests harbor higher levels of endemism than the lowland ecoregion. Half of Sri Lanka's endemic flowering plants and 51 percent of the endemic vertebrates are limited to this ecoregion. The smaller, isolated Knuckles Range has several species of relict, endemic flora and fauna that are distinct from the montane forests of the central massif (Senanayake et al. 1977). More than 34 percent of Sri Lanka's endemic trees, shrubs, and herbs are limited to the montane rain forests (Peeris 1975 in Gunatilleke and Gunatilleke 1990) represented by this ecoregion. The ecoregion harbors eight near-endemic mammals, and five are strict endemics (table 1). Two genera, Srilankamys and Feroculus, are monotypic and are strictly endemic to this ecoregion. Table 1. Endemic and Near-Endemic Mammal Species.
This ecoregion also supports a population of the Sri Lankan leopard (Panthera pardus kotiya) recognized by IUCN (1996) as a threatened genotype. The leopard is also the largest carnivore in Sri Lanka. Other endangered species include the endemic Rattus montanus and five shrews: Crocidura miya, Feroculus feroculus, Solisorex pearsoni, Suncus fellowsgordoni, and Suncus zeylanicus (IUCN 2000). The Sri Lanka Montane Rain Forests [IM0155] ecoregion is included within an EBA, Sri Lanka (124) (Stattersfield et al. 1998). The ecoregion harbors twenty near-endemic bird species, of which five are strict endemics (table 2). Table 2. Endemic and Near-Endemic Bird Species.
Despite years of biological exploration, new species are still being discovered in this ecoregion, especially within the concealed fauna, such as the frogs, lizards, fishes, and crabs. In addition to the large number of Rhacophorid frogs (Pethiyagoda and Manamendra-Arachchi 1998a), new species have been added to the endemic agamid lizard genera, Lyriocephalus, Ceratophora, and Cophotis, over the past few years (Pethiyagoda and Manamendra-Arachchi 1998b). Dedicated surveys of the crab fauna have increased the number of described species from seven in 1993 to thirty-five, some of which represent endemic genera (WHT 2000). Undoubtedly many more of these secretive yet fascinating species await discovery in this ecoregion.  Current Status
Over the past 200 years, most of the montane rain forests have been cleared to establish large tea (Camellia sinensis) plantations (Ashton et al. 1997). Therefore, we will never know the full extent of the endemic biodiversity that has been lost forever, although the localized distribution patterns of species provide some indication of what this ecoregion's forests may have held. Because many of the endemic species have specialized habitat needs and small spatial needs, even small habitat fragments can provide viable habitat for many of the ecoregion's species that are key to its biodiversity. Therefore, protecting the remaining forest patches and their natural biodiversity is imperative. Currently, the ecoregion has five protected areas-of which one (Peak Wilderness) extends partially into the ecoregion from the lowland rain forests ecoregion-that cover less than 500 km2 (table 3). But none have good protection measures or conservation plans in place. Table 3. WCMC (1997) Protected Areas That Overlap with the Ecoregion.
In addition to instituting good management in existing reserves, an attempt should be made to link the forest patches that are contiguous with the lowland and submontane forests to create more effective conservation landscapes across the altitudinal gradient. Because the major rivers originate in the mountains and radiate outward, the altitudinal connectivity will protect the watersheds and stabilize the substrate. The frequent landslides that result in loss of life and property are a manifestation of the loss of ground cover in these montane forests. Failure to act soon will result in the loss of Sri Lanka's most valuable contribution to global conservation. The primary threats are from land clearing for plantations, agriculture, and illegal logging (Gunatilleke and Gunatilleke 1990), even within protected areas. Most of the natural habitat has already been cleared for large-scale tea plantations, but the few remaining patches are still being cleared for other agricultural crops. Mining for precious stones have devastated large areas of forests. The cloud forests in the high montane areas, especially in the Horton Plains National Park, are experiencing diebacks. Investigations are under way to determine the causes. In the Knuckles Range the undergrowth in large forest areas is being cleared for cardamom (Elettaria cardamomum) plantations (IUCN 1994). Therefore, the regeneration capacity of these forests-though seemingly intact because of the intact canopy-is highly compromised.
Sri Lanka's forests have been divided into two broad climatic sub-regions: the wet zone and the dry zone. In a previous analysis of conservation units of the Indo-Malayan realm, MacKinnon (1997) placed the wet-zone forests into a single biounit, Ceylon Wet Zone 02. We used MacKinnon's regional classification as a guiding framework in delineating ecoregions across the Indo-Pacific region. But because we differentiated between lowland and montane forests in delineating ecoregions, we used the 1,000-m contour to extract and place the montane rain forests into a distinct ecoregion: the Sri Lanka Montane Rain Forests [IM0155]. This ecoregion includes the montane floristic zones (9, 10, 12, 13, 14, and 15) identified by Ashton and Gunatilleke (1987).
References for this ecoregion are currently consolidated in one document for the entire Indo-Pacific realm. Reviewed by: This text was originally published in the book Terrestrial ecoregions of the Indo-Pacific: a conservation assessment from Island Press. This assessment offers an in-depth analysis of the biodiversity and conservation status of the Indo-Pacific's ecoregions. For more general information on this ecoregion, go to the WildWorld version of this description. All text by World Wildlife Fund © 2001 | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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