Intra‐lake stable isotope ratio variation in selected fish species and their possible carbon sources in Lake Kyoga (Uganda): implications for aquatic food web studies

The stable isotopes of nitrogen (δ¹⁵N) and carbon (δ¹³C) provide powerful tools for quantifying trophic relationships and carbon flow to consumers in food webs; however, the isotopic signatures of organisms vary within a lake. Assessment of carbon and nitrogen isotopic signatures in a suite of plants, invertebrates, and fishes in Lake Kyoga, indicated significant variation between two sites for δ¹³C (paired t = 6.305; df = 14, P < 0.001 and δ¹⁵N paired t = 1.292; df = 14; P < 0.05). The fish fauna in Bukungu was generally more ¹³C enriched (mean δ¹³C = –16.37 ± 1.64‰) than in Iyingo (mean δ¹³C = –20.80 ± 2.41‰) but more δ¹⁵N depleted (mean δ¹⁵N = 5.57 ± 0.71‰) than in Iyingo (mean δ¹⁵N = 6.92 ± 0.83‰). The simultaneous shifts in phytoplankton and consumer signatures confirmed phytoplankton as the major source of carbon for the food chain leading to fish. Limited sampling coverage within lakes may affect lake wide stable isotope signatures, and the same error is transferred into trophic position estimation. Consideration of potential intra‐lake spatial variability in isotope ratios and size is essential in evaluating the spatial and trophic structure of fish assemblages.