“…Although N is the most limiting nutrient in many tundra communities, P limitation is also widespread (Barel & Barsdate, 1978), particularly for the growth of Friophorum (Tamm, 1954;Shaver & Chapin 1995), Any changes in root POj^" uptake capacity might have a significant impact on Friophorum and therefore on tundra responses to elevated CO., Root POj^^ uptake requires expenditure of respiratory energy (Mengel & Kirkby, 1978;Bieleski & Ferguson, 1983), Because CO^ enrichment often enhances root supply of carbohydrate substrates for respiration (Tschaplinski, Norby & Wullschleger, 1993;BassiriRad et al, 1996), we hypothesized that elevated CO., might lead to increased root PO4^" uptake. Soil temperature has a marked effect on uptake of all macronutrients (Clarkson, Hopper & Jones, 1986), including PO^'*" uptake in Friophorum (Chapin, 1977;Chapm, Van Cleve & Chapin, 1979) and other species (Jeschke & Simonis, 1965 ;Sutton, 1969), The effect of root temperature on ion uptake is likely to be regulated via changes in root import of photoassimilates and respiration rate (Farrar, 1988), Therefore, we also hypothesized that the nature and the magnitude of changes in PO,,^" uptake at high CO, would depend on soil temperature. The effects of soil temperature are of particular importance in the Arctic because global warming is expected to be more pronounced at high latitudes (Lashof & Ahuja, 1990;Maxwell, 1992), and models predict that arctic soil temperatures will closely track the increase in air temperature (Kane et al, 1992),…”