NONMYCORRHIZAL UPTAKE OF AMINO-ACIDS BY ROOTS OF THE ALPINE SEDGE KOBRESIA MYOSUROIDES - IMPLICATIONS FOR THE ALPINE NITROGEN-CYCLE

Non-mycorrhizal plants of the alpine sedge, Kobresia myosuroides, take up the amino acid glycine from nutrient solutions at greater rates th an NO3- or NH4+. The amino acids glutamate and proline were also taken up at high rates. Total plant biomass was twice as high after 4 month s of growth on glycine, compared to NH4NO3, with significant increases in both root and leaf biomass. By taking advantage of differences in the delta(13)C signature of air in the growth chamber and the glycine used for growth , a two-member mixing model was used to estimate that a significant amount of the glycine was taken up as intact molecules, enough to contribute 16% of the total carbon assimilation over a 4-mon th growing period. Glycine uptake was inhibited when roots were expose d to N-2 in place of air, and when the protonophore carbonyl cyanide m -chlorophenylhydrazone (CCCP) was added to the rood solution. From the se results it is concluded that glycine uptake occurs through active t ransport. Glycine uptake exhibited a Q(10) of 2.0 over the temperature range 5-15 degrees C C, with relatively high rates maintained at the lowest temperature measured (5 degrees C). Roots of Kobresia were not capable of taking up NH4+ at measureable rates. To our knowledge, this is the first report of a plant whose non-mycorrhizal roots cannot tak e up NH4+. Measurements of three N fractions (No-3(-), NH4+, and total amino acids) in the soil pore water were made over total amino acids) in the soil pore water were made over two growing seasons in two Kobr esia dry meadows using microlysimeters. At the West Knoll site, which is characterized by soils with average amounts of organic matter, the dominant forms of N in the soil pore water were NO3 and NH4+ (0-450 mu mol L. amino acid concentrations were generally less than 20 mu mol L (-1) at his site. At the East Knoll site, which is characterized by so ils with higher than average amounts of organic matter, amino acids we re generally present at higher concentrations (17-100 mu mol L(-1)), c ompared to No-3(-) and NH4+. The most abundant amino acids were glycin e (10-100 mu mol L(-1)), glutamate (5-70 mu mol L(-1)), and late in th e season cysteine (5-15 mu mol L(-1)). The results demonstrate that th is sedge, which dominates dry meadow communities in many alpine ecosys tems, is capable of taking up intact amino acids as a principal N sour ce, and has access to high amino acid concentrations in certain alpine soils. Such uptake of organic N may accommodate plant N demands in th e face of slow alpine N mineralization rates due to cold soil temperat ures.