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in Sri Lanka - Ministry of Environment

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Present status <strong>of</strong> Lowland Wet Zone Flora <strong>of</strong> <strong>Sri</strong> <strong>Lanka</strong>H. S. KathriarachchiDepartment <strong>of</strong> Plant Sciences, University <strong>of</strong> ColomboIntroduction<strong>Sri</strong> <strong>Lanka</strong> has an outstand<strong>in</strong>g biodiversity because <strong>of</strong> its tropical climate, soil, topographicalvariations, geographical location and its strik<strong>in</strong>g biogeographic history. Together with theWestern Ghats <strong>in</strong> India, <strong>Sri</strong> <strong>Lanka</strong> is considered as one <strong>of</strong> the 34 biodiversity hotspots <strong>in</strong>the world because <strong>of</strong> the high degree <strong>of</strong> endemism <strong>in</strong> fauna and flora and serious amount <strong>of</strong>habitat loss (Ashton et al., 1997; Gunatilleke et al., 2004). The diverse array <strong>of</strong> ecosystems <strong>in</strong><strong>Sri</strong> <strong>Lanka</strong> harbors a wealth <strong>of</strong> plant species and they provide a habitat for many other speciesas yet undiscovered.<strong>Sri</strong> <strong>Lanka</strong> also has a diversity <strong>of</strong> climatic and floristic regions show<strong>in</strong>g spatial variations <strong>in</strong> ra<strong>in</strong>fall,altitude and soil. Lowland wet zone represents the area below 1,000 m <strong>in</strong> elevation, spread<strong>in</strong>g<strong>in</strong> the southwestern quarter <strong>of</strong> <strong>Sri</strong> <strong>Lanka</strong> (Figure 1), ma<strong>in</strong>ly <strong>in</strong> the Colombo, Gampaha, Kalutara,Galle, Matara, Kegalle districts and part <strong>of</strong> Ratnapura (Gunatilleke and Ashton, 1987b; M<strong>in</strong>istry<strong>of</strong> Forestry and <strong>Environment</strong>, 1999).Flora <strong>of</strong> the lowland wet zone <strong>of</strong> <strong>Sri</strong> <strong>Lanka</strong> is largely distributed <strong>in</strong> the tropical lowland ra<strong>in</strong>forests- forests below 1,000 m altitude (Figure 1). These forests have an aseasonal wet climate andgenerally receive 2500 – 5000 mm <strong>of</strong> mean annual ra<strong>in</strong> fall without prom<strong>in</strong>ent dry spells. Meanannual temperature is about 27 o C at sea level. The lowland wet zone forests are classified byde Rosayro (1950) as wet evergreen forest climax by Koelmeyer (1957) and Holmes (1956) aswet tropical evergreen forests . These forests are conf<strong>in</strong>ed to 2.14% (141,506 ha) <strong>of</strong> the totalland area <strong>of</strong> <strong>Sri</strong> <strong>Lanka</strong> (M<strong>in</strong>istry <strong>of</strong> Forestry and <strong>Environment</strong>, 1999).SRIFigure. 1 Map show<strong>in</strong>g the forests <strong>in</strong> the south-west <strong>of</strong> <strong>Sri</strong> <strong>Lanka</strong>. Blue = Fragmented lowlandra<strong>in</strong> forests rema<strong>in</strong><strong>in</strong>g <strong>in</strong> <strong>Sri</strong> <strong>Lanka</strong>, Green = Montane ra<strong>in</strong> forests, Brown = Intermediate zone forests,Yellow = Dry zone forests (Source: Somasekaram et al., 1997).175

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