Limnology of Parakrama Samudra — Sri Lanka 1983
DOI: 10.1007/978-94-009-7281-0_6
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Some remarks on long-term and seasonal changes in the zooplankton of Parakrama Samudra

Abstract: A study of zooplankton samples taken from Parakrama Samudra revealed long-term changes in species composition. However, these changes were probably due to low water levels following a catastrophic cyclone in 1978. Species composition seems to have returned to a stable condition after restoration of high water levels. Seasonal changes in composition and densities of plankton were not marked over a three-years sampling period.

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Cited by 16 publications
(10 citation statements)
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“…Similar trend has been recorded in several other water bodies in Sri Lanka including Randenigala (Pathmalal and Piyasiri 1999) and Kotmale (Piyasiri and Chandrananda 1998) reservoirs in the central highlands, Bolgoda (Wignarajah and Amarasiriwardene 1983) and Beira (Kamaladasa and Jayatunga 2007) lakes in the western coastal region of the wet zone and Parakrama Samudra in the low country dry zone (Fernando and Rajapakse 1983). However, Wickramasinghe et al (2012) recorded lesser number of species of cladocerans than that of copepods in an urban wetland in the wet zone of Sri Lanka.…”
Section: Discussionsupporting
confidence: 48%
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“…Similar trend has been recorded in several other water bodies in Sri Lanka including Randenigala (Pathmalal and Piyasiri 1999) and Kotmale (Piyasiri and Chandrananda 1998) reservoirs in the central highlands, Bolgoda (Wignarajah and Amarasiriwardene 1983) and Beira (Kamaladasa and Jayatunga 2007) lakes in the western coastal region of the wet zone and Parakrama Samudra in the low country dry zone (Fernando and Rajapakse 1983). However, Wickramasinghe et al (2012) recorded lesser number of species of cladocerans than that of copepods in an urban wetland in the wet zone of Sri Lanka.…”
Section: Discussionsupporting
confidence: 48%
“…The number of species of zooplankton recorded in a single reservoir during the present study was less than those recorded for many other reservoirs in Sri Lanka including Parakrama Samudra (Fernando and Rajapakse 1983), Kalawewa (Jayatunga 1986), Giritale (Cooray and Jayatunga 2000), Randenigala (Pathmalal and Piyasiri 1999), Kotmale (Piyasiri and Chandrananda), and Victoria (Piyasiri and Jayakody 1991) reservoirs. Of these, the latter three reservoirs are highland reservoirs which are classified as oligo-mesotrophic (Rott et al 2008).…”
Section: Discussionmentioning
confidence: 56%
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“…Similar results were obtained in Prakrama Samudra by Fernando & Rajapaksa in 1983. They have recorded 32 species of Rotifers, 7 species of Cladocerans, 6 species of Copepods and 4 species of Protozoans etc.…”
Section: Discussionsupporting
confidence: 84%