Untersuchungen �ber die Raten der Polyphosphatsynthese durch die Photophosphorylierung bei Ankistrodesmus braunii

Abstract

Short-time experiments with 32P-labelled phosphate and chase experiments with equally labelled cells were carried out with synchronized algae under conditions of optimum phosphate uptake. In short-time experiments, in the presence as in the absence of CO2, orthophosphate and organic phosphates are rapidly labelled, but their time curves show saturation behaviour after 10 to 20 min. Labelling of polyphosphates proceeds at a constant rate after a short lag period of about 5 min. In equally labelled algae 32P-labelling correspondingly decreases in orthophosphate and in organic phosphates, but increases by about the same amount in the fraction of acid-insoluble polyphosphates. In the presence of external phosphate and in the light, polyphosphates show no visible decay within the 20 min of the chase experiments. A comparison of the two kinds of experiments suggests that polyphosphates are secondary products of photophosphorylation following only after orthophosphate and organic phosphates, probably after ATP. The rates of photophosphorylation are certainly much higher than the rates of labelling in organic phosphates because of the limiting phosphate uptake. Since the polyphosphates show no decay during the time of the experiments their turnover is low and the rates of polyphosphate labelling after a phosphate starvation period, and after the short lag period, can be regarded as approximate rates of polyphosphate synthesis. These rates are lower than the rates of phosphate uptake. In young cells of the synchronous culture phosphate replenishment after a 5-h starvation requires 2 to 3 h. After replenishment or in a culture undisturbed by phosphate starvation, the rates of polyphosphate accumulation, like the rates of phosphate uptake are much lower. In the presence of CO2 they are constant for several hours, if related to culture volume with constant cell number. Polyphosphate accumulation is proportional to phosphate uptake under these conditions amounting to about one third. In the absence of CO2, the rates decrease after 2 to 4 h of CO2-starvation and, like in short-time experiments a large proportion of the phosphate taken up is used for polyphosphate accumulation. The low rates of long-time experiments may represent a steady state between formation and decay of polyphosphates. Since the cells kept in the absence of CO2 are prevented from growing they actually accumulate more polyphosphates per cell volume, per chlorophyll, and per dry weight than the cells in the presence of CO2. The rates of polyphosphate formation are discussed with respect to their turnover in the light observed by other investigators. They are regarded to be a result of competition for ATP together with the orthophosphate pool of the cells, and of the compartmentation. The rates of polyphosphate formation are rather low compared with the probable rates of ATP formation under various conditions of photophosphorylation. Therefore, the formation of polyphosphates is regarded as a process of secondary order of magnitude in the energy metabolism of algal cells.