LIFAHAMU ZIWA VICTORIA KIUNDANI

Lake Victoria

Lake Victoria has a surface area of about 68,000 km2 equal to the size of Ireland and it is the largest of Africas lakes as well as the largest tropical lake in the world.

View over Lake Victorias Winam Gulf with Kisumu Impala Sanctuary in the foreground

Lake Victoria is the second largest freshwater lake in the world if Michigan-Huron are counted as two separate lakes. In 1858, John Hanning Speke was the first European to explore the vast lake and he believed it to be the source of the White Nile. The assertion was ridiculed until Henry Morton Stanley eventually proved him right in 1875.

The lake basin is not a part of Great Rift Valley and its long line of lakes such as Lake Tana, Lake Naivasha, Nakuru, Elementeita, Lake Tanganyika, Lake Malawi and others. Therefore Lake Victoria is quite shallow with an average depth of about 30-40m and a maximum depth of 81 meters and Kenya actually owns only a tiny 3,785 sq km corner of the lake

Lake Victoria, the largest tropical lake in the world, suffers from severe eutrophication and the probable extinction of up to half of its 500+ species of endemic cichlid fishes. The continuing degradation of Lake Victoria's ecological functions has serious long-term consequences for the ecosystem services it provides, and may threaten social welfare in the countries bordering its shores. Evaluation of recent ecological changes in the context of aquatic food-web alterations, catchment disturbance and natural ecosystem variability has been hampered by the scarcity of historical monitoring data. Here, we present high-resolution palaeolimnological data, which show that increases in phytoplankton production developed from the 1930s onwards, which parallels human-population growth and agricultural activity in the Lake Victoria drainage basin. Dominance of bloom-forming cyanobacteria since the late 1980s coincided with a relative decline in diatom growth, which can be attributed to the seasonal depletion of dissolved silica resulting from 50 years of enhanced diatom growth and burial. Eutrophication-induced loss of deep-water oxygen started in the early 1960s, and may have contributed to the 1980s collapse of indigenous fish stocks by eliminating suitable habitat for certain deep-water cichlids. Conservation of Lake Victoria as a functioning ecosystem is contingent upon large-scale implementation of improved land-use practices.