Terrestrial exports of protons (H + ), nitrate (NO 3 − ), dissolved organic carbon including organic acid anions (A − ), phosphorus (P), base cations, and ionic aluminum (Al i ) underwent pronounced changes after bark beetle-induced tree dieback (2004)(2005)(2006)(2007)(2008) in a nitrogen-saturated, chronically acidified but recovering catchment, Plešné Lake, Czech Republic. After a short decline in lake water pH immediately after tree dieback, the ecosystem recovery from acidification accelerated and the carbonate buffering system was restored by 2011, after $ 6 decades of depletion by acid rain. Major reasons for this rapid transition were changes in intensity of in-lake biogeochemical (H + producing/removing) processes caused by changing concentrations and proportions of solutes exported from soil to surface water. In-lake denitrification, elevated NO 3 − assimilation (due to elevated P input), and photochemical/ microbial oxidation of A − were the most important H + removing processes, while Al i hydrolysis was the most important H + source. Phytoplankton biomass increased with elevated P inputs and increasing P availability, which resulted from reduced in-lake formation of Al hydroxide (and thus less adsorption of P) and more intensive P recycling by zooplankton. The rapidly changing lake water chemistry and elevated P availability after tree dieback in the catchment thus have enabled further biological recovery of Plešné Lake.