Seasonal variations in the stable isotope composition (␦ 13 C and ␦ 15 N) of crustacean zooplankton and their putative food sources in oligotrophic Loch Ness were recorded during 1998. Bulk particulate organic matter (POM) showed ␦ 13 C values consistent with a terrestrial plant origin from the catchment and exhibited little seasonal variation, whereas POM ␦ 15 N was more variable, probably due to associated microbial action. In contrast, phytoplankton ␦ 13 C was relatively light and showed some seasonal variation, but ␦ 15 N values were more constant. The isotopic signatures of both POM and phytoplankton remained sufficiently distinct from each other throughout the period of study to allow their relative contributions to zooplankton diet to be assessed. Zooplankton isotopic signatures shifted seasonally, reflecting a dietary switch from a reliance on allochthonous carbon derived from POM during winter and early spring to heavy dependence on algal production during summer. Annually, crustacean zooplankton in Loch Ness derive approximately 40% of their body carbon from allochthonous sources, likely mediated via microbial links. Separate determination of isotope ratios for the main zooplankton species allowed a more detailed trophic investigation. The most abundant zooplankton species in the loch, Eudiaptomus gracilis, incorporated appreciable allochthonous carbon even during the peak of phytoplankton productivity. By contrast, Daphnia hyalina grew mainly in late summer and autumn and derived almost 100% body carbon from algal sources. This study is the first to quantify such a seasonal switch in zooplankton dependence between allochthonous and autochthonous sources of organic matter in a large lake.The ecological importance of terrestrially derived material to lake food webs is receiving increasing attention. Much of the impetus for this has come from studies of the dark stained waters of small, boreal forest lakes of Scandinavia resulting from humic matter originating in the catchment (Meili 1992). The staining restricts light penetration into the water column and presents an unfavorable environment for photosynthetic fixation of carbon in situ by autotrophic phytoplankton (Jones 1992). Thus, in these systems, autochthonous production is usually very low. Humic material is capable of supporting bacterial metabolism (Hessen 1992) and associated heterotrophic organisms in the microbial loop (Tranvik 1992); consequently, a significant contribution to the humic lake food web may be derived from allochthonous matter via detritus-driven food chains. Jones (1992) hypothesized that the relative importance of allochthonous organic matter to the pelagic food web of lakes should increase with decreasing lake trophy, and a survey of the balance between planktonic production : respiration ratios lent support to this hypothesis (del Giorgio andPeters 1993, 1994). In oligotrophic lakes where community respiration equals or exceeds phytoplankton production (del Giorgio et al. 1997), the heterotrophic plankton must recei...