ABSTRACT
Variations of δ13C and δ15N in dissolved organic matter and size-fractionated plankton, ranging from 0.7 to 200 μm, were studied in Taihu Lake on two occasions during a cyanobacterial bloom. Paired-sample t-tests indicated that stable isotope ratios of samples collected did not significantly differ from each other on the two sampling dates. The overall correlation between δ13C and δ15 of forty taxa of the plankton community was weak (r2=0.227, N=40), indicating a non-trophic enrichment effect in δ13C. The δ15N values increased along with plankton size. We used δ15 as an index of the trophic level and demonstrated that logarithmic organism size was positively and significantly related to trophic level, indicating that a size-dependent approach is preferable in the analysis of trophic isotope enrichment in microplankton food webs.