Bythotrephes cederströemi have invaded numerous inland lakes in North America, many of which are strati ed and support offshore shes like the Cisco (Coregonus artedi). While evaluations based on changes in zooplankton community composition following Bythotrephes invasion predict an increase in Cisco mercury concentrations, this phenomenon was not detected from a survey evaluating temporal changes in Cisco Hg across a broad range of lakes varying in the presence or absence of Bythotrephes. Here, we compare temporal changes in Cisco biomagni cation factor slopes (i.e., slopes of relationships between Cisco Hg and δ 15 N isotopes) from lakes experiencing Bythotrephes invasion over the study period to those already invaded (as a reference) over similar time periods. Our results show that biomagni cation slopes after Bythotrephes invasion either changed direction entirely (from positive to negative relationships) or decreased in elevation relative to those prior to invasion. No such pattern was observed in previously invaded reference lakes. Reductions in Cisco biomagni cation slopes and/or intercepts following Bythotrephes invasion suggest that conversion e ciency (and therefore growth) of Cisco increased after invasion (i.e., less Hg accumulates in sh at an equivalent trophic position after vs. before invasion). Back-calculated Cisco growth rates and size-at-age were greater in the presence of Bythotrephes than without, further supporting the hypothesis that changes in Hg biomagni cation are likely due to increased conversion e ciency. These ndings highlight the potential importance of foraging energetics over and above shifts in trophic position in modifying sh contaminant concentrations.