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PLANT PHYSIOLOGY , Vol 110, Issue 3 773-779, Copyright © 1996 by American Society of Plant Biologists
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WHOLE PLANT, ENVIRONMENTAL, AND STRESS PHYSIOLOGY |
Kinetics of NH4+ Influx in Spruce
H. J. Kronzucker, M. Y. Siddiqi and ADM. Glass
Department of Botany, University of British Columbia, Vancouver, British Columbia, Canada V6T 1Z4
Influxes of 13NH4+ across the root plasmalemma were measured in intact
seedlings of Picea glauca (Moench) Voss. Two kinetically distinct uptake
systems for NH4+ were identified. In N-deprived plants, a
Michaelis-Menten-type high-affinity transport system (HATS) operated in a
2.5 to 350 [mu]M range of external NH4+ concentration ([NH4 +]o). The Vmax
of this HATS was 1.9 to 2.4 [mu]mol g-1 h-1, and the Km was 20 to40 [mu]M.
At [NH4+]o from 500 [mu]M to 50 mM, a linear low-affinity system (LATS) was
apparent. Both HATS and LATS were constitutive. A time-dependence study of
NH4+ influx in previously N-deprived seedlings revealed a small transient
increase of NH4+ influx after 24 h of exposure to 100 [mu]M [NH4+]o. This
was followed by a decline of influx to a steady-state value after 4 d. In
seedlings exposed to 100 [mu]M external NO3- concentration for 3 d, the
Vmax for NH4+ uptake by HATS was increased approximately 30% compared to
that found in N-deprived seedlings, whereas LATS was down-regulated. The
present study defines the much higher uptake capacity for NH4+ than for
N03- in seedlings of this species.
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