Mass Flux Calculations Show Strong Allochthonous Support of Freshwater Zooplankton Production Is Unlikely
Figure 3
The influence of t-DOC loading and retention on absolute and available t-DOC fluxes.
The absolute t-DOC loading values are from Fig. 2B. The available t-DOC flux was calculated as the absolute flux multiplied by the corresponding in-lake t-DOC retention from Fig. 2C, i.e., (areal t-DOC loading)*(σ/(σ + ρ)).