Regulation of intracellular pH values in higher plant cells. Carbon-13 and phosphorus-31 nuclear magnetic resonance studies.

The regulation of the cytoplasmic and vacuolar pH values (pHc and pHv) in sycamore (Acer pseudoplatanus L.) cells was analyzed using 31P and 13C nuclear magnetic resonance spectroscopy. Suspension-cultured cells were compressed in the NMR tube and perfused with the help of an original arrangement enabling a tight control of the pH (external pH, pHe) of the carefully oxygenated circulating nutrient medium. Intracellular pH values were measured from the chemical shifts of: CH2-linked carboxyl groups of citric acid below pH 5.7; orthophosphate between pH 5.7 and 8.0; 13C-enriched bicarbonate over pH 8.0. pHc and pHv were independent of pHe over the range 4.5-7.5. In contrast intracellular pH values decreased rapidly below pHe 4.5 and increased progressively at pHe over 7.5. There was an acceleration in the rate of O2 consumption accompanied with a decrease in cytoplasmic ATP concentration as pHe decreased. When the rate of O2 consumption was approaching the uncoupled O2 uptake rate, a loss of pHc control was observed. It is concluded that as pHe decreased, the plasma membrane ATPase consumed more and more ATP to reject the invading H+ ions in order to maintain pHc at a constant value. Below pHe 4.5 the efficiency of the H+ pump to react to back leakage of H+ ions became insufficient, leading to an acidification of pHc and to an alkalinization of pHe. On the other hand, over pHe 7.5 a passive influx of OH- ions was observed, and pHc increased proportionally to the increase of pHe. Simultaneously appreciable amounts of organic acids (malate and citrate) were synthesized by cells during the course of the alkalinization of the cytoplasmic compartment. The synthesis of organic acids which partially counteract the alkalinization of the cytoplasmic compartment may result from a marked activation of the cytoplasmic phosphoenolpyruvate carboxylase induced by an increase in cytoplasmic bicarbonate concentration. The fluctuations of pHv followed a similar course to that of pHc. It is concluded that the vacuole, which represents a potentially large H+ ions reservoir, can counteract H+ (or OH-) ion invasion observed at acidic (or alkaline) pHe contributing to the homeostasis of pHc.