PLANT PHYSIOLOGY , Vol 111, Issue 1 93-100, Copyright © 1996 by American Society of Plant Biologists
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WHOLE PLANT, ENVIRONMENTAL, AND STRESS PHYSIOLOGY |
Direct Measurement of 59Fe-Labeled Fe2+ Influx in Roots of Pea Using a Chelator Buffer System to Control Free Fe2+ in Solution
T. C. Fox, J. E. Shaff, M. A. Grusak, W. A. Norvell, Y. Chen, R. L. Chaney and L. V. Kochian
United States Plant Soil and Nutrition Laboratory, United States Department of Agriculture-Agricultural Research Service (USDA-ARS), Cornell University, Ithaca, New York 14853 (T.C.F., J.E.S., W.A.N., L.V.K.)
Fe2+ transport in plants has been difficult to quantify because of the
inability to control Fe2+ activity in aerated solutions and non-specific
binding of Fe to cell walls. In this study, a
Fe(II)-3-(2-pyridyl)-5,6-diphenyl-1,2,4-triazine-4[prime]4"-disulfonic acid
buffer system was used to control free Fe2+ in uptake solutions.
Additionally, desorption methodologies were developed to adequately remove
nonspecifically bound Fe from the root apoplasm. This enabled us to
quantify unidirectional Fe2+ influx via radiotracer (59Fe) uptake in roots
of pea (Pisum sativum cv Sparkle) and its single gene mutant brz, an Fe
hyperaccumulator. Fe influx into roots was dramatically inhibited by low
temperature, indicating that the measured Fe accumulation in these roots
was due to true influx across the plasma membrane rather than nonspecific
binding to the root apoplasm. Both Fe2+ influx and Fe translocation to the
shoots were stimulated by Fe deficiency in Sparkle. Additionally, brz, a
mutant that constitutively exhibits high ferric reductase activity,
exhibited higher Fe2+ influx rates than +Fe-grown Sparkle. These results
suggest that either Fe deficiency triggers the induction of the Fe2+
transporter or that the enhanced ferric reductase activity somehow
stimulates the activity of the existing Fe2+ transport protein.