P. Lim et al., Diversity and spatial distribution of freshwater fish in Great Lake and Tonle Sap river (Cambodia, Southeast Asia), AQU LIV RES, 12(6), 1999, pp. 379-386
Fish catches around the Great Lake, Tonle Sap river and the transitional zo
ne between the lake and the river were studied by professional 'fishing lot
' (i.e. fishing zone) from 1995 to 1997. One hundred and twenty species of
fish, belonging to 26 families and nine different orders were recorded. Com
pared to previous studies (1936-1976), only 53 % of families, 32 % of gener
a and 54 % of species were collected by professional fishing lot. This impo
rtant loss in biodiversity could have several causes: bias of sampling proc
edures between professional fishing and research sampling, overfishing, mod
ification of the floodplain by deforestation, etc. The professional fishing
data showed that Cypriniformes accounted for 41.6 % of the total number of
individuals caught, the Cyprinidae family alone represented 40 species. Si
luriformes made up 21.6 %, Perciformes 13.3 %, with six other orders repres
ented by smaller numbers. Eighty-seven percent of the recorded species occu
r in both habitats depending on the season. Migration takes place from the
Mekong river to the Gnat Lake through the Tonle Sap river at the beginning
of the rainy season (May-October), and in the reverse direction at the star
t of the dry season (November-February). The majority of the species reprod
uce at the start of the rainy season (May-June) in the hooded plain and the
forest floodplain of the Great Lake: the period, the place and the means o
f reproduction have not been closely studied, particularly for the Belontif
ormes, Clupeiformes, Synbranchiformes, Pleuronectiformes and Tetraodontifor
mes. Multivariate analysis of fishing data (November-February) shows three
distinct communities: that of the lake (Perciformes and Siluriformes), of t
he river (Pleuronectiformes, Cypriniformes, Clupeiformes and Siluriformes),
and of the transitional zone formed from the principal channel, the old ri
ver channel and the oxbow lakes (Cypriniformes, Siluriformes and Osteogloss
iformes). (C) 1999 Ifremer/Cnrs/lnra/lrd/Cemagref/Editions scientifiques et
medicales Elsevier SAS.