Titlebook: Environmental Change and Response in East African Lakes; John T. Lehman Book 1998 Springer Science+Business Media Dordrecht 1998 Ecology.E

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: Spatial Distribution and Egg Production in Lake Victoria, Ugandahe full water column of the lake, with most individuals close to the bottom during day time and most distributed throughout all lake depths during the night. Diel vertical migration by . occurs at all lake regions, but it is most pronounced at deep, offshore locations. In offshore regions, . populat

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Low-Oxygen Tolerance of the Atyid Prawn, ,, in Lake Victoria (East Africa): Implications for Refuge d state is the potential loss of habitat for fishes and invertebrates that are sensitive to hypoxia. Laboratory experiments with the meroplanktonic prawn, ., show that survivorship and body growth are not significantly different between animals reared under low-oxygen conditions (3–4 mg L. O. and th

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Secondary Production by the Lake Fly , in Lake Victoria, East Africa: Implications for Trophic Dynambrate predator and forage item for planktivorous fish. We incorporated in situ development times and length-weight relationships of larvae and pupae collected from offshore waters throughout 1994. The model predicted . biomass to be 55 mg C m. during 1994 with a production to biomass ratio of 0.11 d

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Nutrients and Plankton Biomass in the Rift Lake Sources of the White Nile: Lakes Albert and Edwarder column chemistry, plankton biomass, and production rates. Biomass of phytoplankton exceeds that of zooplankton in both rift lakes, and the predictive relationship between light attenuation and particulate chlorophyll is consistent with that of Lake Victoria. Cyclopoid copepods dominate Albert and

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Comparison of Isotopic Records in Abiogenic and Biogenic Calcite from Lake Turkana, Kenyae. The carbonates appear to form out of equilibrium with the modern lake waters. The micrite is precipitating at 0.6‰ to 2‰ below equilibrium values whereas the ostracods are forming their shells at 0.3‰ to 2.0‰ above equilibrium. This seems to be caused by the extent of interaction between inflow a

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0077-0639 at exist within IDEAL. This book follows in the spirit of The Limnology, Climatology, and Paleoclimatology of the East African Lakes, published in 1996, but has978-90-481-5043-4978-94-017-1437-2Series ISSN 0077-0639 Series E-ISSN 2215-1729

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