This paper examines why turbulent tracer fluxes can depend on gradients elsewhere in space and earlier in time. It develops a formal expression for that dependence as a nonlocal functional of the mean tracer gradient. Two-dimensional turbulence simulations, stochastic velocity fields, and iterated maps reveal the extent and structure of the resulting transport kernels. The analysis identifies circumstances in which a local eddy diffusivity is a reasonable approximation and cases where it misses important transport effects. Readers get a framework for diagnosing nonlocality and using it to guide the design of physically informed, data-driven mixing parameterizations.