“…We applied nutrient treatments to dry soil prior to watering to minimize leaching from oversaturated soils, although actual soil nitrogen and phosphorus concentrations may have been lower due to plant use. The nitrogen concentrations were chosen to reflect low and high measurements of reactive soil nitrogen (NH 4 + NO 3 ; about 10–225 ppm μg N·g −1 soil; Van Cleve and Alexander, ; Gordon et al., ; Van Cleve et al., ; Yarie, ; Clein and Schimel, ; Stottlemyer et al., ; Jerabkova et al., ; Bales and Hersch‐Green, ), and the soil phosphorus concentrations were chosen to reflect the range of available phosphate (PO 4 ) in soil humus layers (about 0.5–100 ppm μg P·g −1 soil; Chapin et al., ; Dyrness et al., ; Yarie, ; Giesler et al., ; Neff et al., ; Stark, ; Hedwall et al., ) reported near our original seed collection sites in interior Alaska and similar ecosystems. We decided to keep relative nitrogen and phosphorus contributions equivalent across nutrient treatments and chose a 10:1 ratio of nitrogen to phosphorus and based the low and high treatments on reported nitrogen levels because nitrogen is more variable and phosphorus tends to occur at low concentrations in Alaskan soils (Chapin et al., ; Van Cleve and Alexander, ; Gordon et al., ; Dyrness et al., ; Van Cleve et al., ; Giesler et al., ; van der Welle et al., ; Jerabkova et al., ; Kielland et al., ).…”