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Plant function and evolutionary biology
RESEARCH ARTICLE

Chloride uptake by oat coleoptile parenchyma described by combined influx and efflux transport systems

Olga K. Babourina, Andrew E. Knowles and Ian A. Newman

Australian Journal of Plant Physiology 25(8) 929 - 936
Published: 1998

Abstract

Chloride fluxes for oat coleoptile parenchyma were measured using the MIFE system for non-invasive microelectrode ion flux measurement. The effects on chloride fluxes of membrane potential, external chloride concentration, pH, cation composition of the bathing solution, and the anion channel blocker anthracene-9-carboxylic acid were studied.

From the experimental data we propose that the step-like appearance of the chloride uptake curve at concentrations higher than 1 mM is due to combined activity of influx and efflux systems. According to this hypothesis the uptake of chloride ions is made by a pH sensitive active transport system with Vmax = 4000 nmol m-2 s-1, Km = 7 mM [Cl-]. Chloride ions are released from the cell through channels with Gaussian type kinetics, the characteristics of which are dependent upon the external bathing solution: Vmax = –2300 nmol m-2 s-1 at 25 mM [Cl-] for CaCl2, and Vmax = –2000 nmol m-2 s-1 at 15 mM [Cl-] for KCl; with both curves having the same width of 17 mM [Cl-].

Key words: Cl- membrane transport, flux kinetics, Avena sativa L.

https://doi.org/10.1071/PP98100

© CSIRO 1998

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