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Plant Physiology 76:403-408 (1984) © 1984 American Society of Plant Biologists Reactions of Corn Root Tissue to Calcium 1Department of Plant Biology, University of Illinois, Urbana, Illinois 61801
Washing corn (Zea mays L.) root tissue in water causes loss of about one-third of the exchangeable Ca2+ over the first 10 to 15 minutes. Upon transfer to K+-containing solutions, the tissue shows a short period of rapid K+ influx which subsequently declines. Addition of 0.1 millimolar Ca2+ decreases the initial rapid K+ influx, but increases the sustained rate of K+ and Cl uptake. It was confirmed (Elzam and Hodges 1967 Plant Physiol 42: 1483-1488) that 0.1 millimolar Ca2+ is more effective than higher concentrations for the initial inhibition, and that Mg2+ will substitute. The inhibition arises from a mild shock affect of restoring Ca2+. With 0.1 millimolar Ca2+ net H+ efflux is blocked for 10 to 15 minutes and the cells are depolarized by about 30 millivolts. However, 1 millimolar Ca2+ rapidly produces increased K+ influx and blocks net H+ efflux for only a few minutes; blockage is preceded by a brief net H+ influx which may restore and increase ion transport by reactivating the plasmalemma H+-ATPase. Stimulation of electrogenic H+-pumping with fusicoccin eliminates the shock responses and minimizes Ca2+ effects on K+ influx. Fusicoccin also strongly decreases Ca2+ influx, but has no effect on Ca2+ efflux. Ice temperatures and high pH decreased Ca2+ efflux, but uncoupler and chlorpromazine did not. It is suggested that the inhibitory and promotive actions of Ca2+ are manifested through decreases or increases in the protonmotive force.
1 Supported by the National Science Foundation (PCM 83-06458) and the United States Department of Energy (AC02-76EV00790).
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