Soil biogeochemical responses to the deposition of anadromous fish carcasses in inland riparian forests of the Pacific Northwest, USA

The historic abundance of salmonids returning to natal streams of the inland Pacific Northwest, USA, may have constituted a major nutrient influx into these commonly oligotrophic ecosystems. Inland ecosystems tend to be warmer and dryer and more nutrient limited than coastal ecosystems; therefore, understanding how these inland conditions influence the soil biogeochemical responses to salmon carcass deposition in riparian forests is a vital step in appropriately mitigating for the loss of this nutrient subsidy. Deposition of salmon carcasses in central Idaho riparian forests resulted in a 480-fold increase in soil nitrogen (N), a sevenfold increase in dissolved organic carbon (C), and a fourfold increase in soil respired CO 2, with significant biogeochemical responses persisting at one year after amendment. Despite these large increases in soil N and C, estimates of soil N and C loading only accounted for 31% and 16% of the fish carcass N and C, respectively. However, the magnitude and persistence of soil biogeochemical responses to the deposition of anadromous fish carcasses in central Idaho attests to the importance of this nutrient subsidy to inland riparian ecosystems of the Pacific Northwest.