| Abstract: | The time course of the appearance in the vacuole of Nitellatranslucens and of Tolypella intricata of tracer from the outsidesolution has been studied over short periods of uptake. Thereare two components of chloride transfer to the vacuole, a fastcomponent linear with time and a second component at longertimes whose behaviour is reasonably well described in termsof a single rate constant for exchange; a constant fractionof the total entry is in the fast component and the apparentrate constant for the second component is proportional to theinflux. In Nitella the path of rapid transfer involves chlorideand sodium, and may also involve a small but variable amountof potassium, but in Tolypella potassium has a significant componentof rapid transfer; these correspond to the cations for whichchloride-linked components of cation influx have been shownby another worker. Over both parts of the time course the level of activity inthe cytoplasm specifies, not the rate of transfer to the vacuoleas would be expected, but the rate as a fraction of the influx;the processes of influx to the cell and transfer to the vacuoleare intimately linked. It is difficult to explain the results in terms of static membranesand fixed compartments. An explanation in terms of the sequence,entry of salt by pino-cytotic vesicles at the plasmalemma, fusionof these vesicles with the endoplasmic reticulum after someloss of tracer to the surrounding cytoplasm, and transfer tothe vacuole in minivacuoles formed from the endoplasmic reticulum,is consistent with the time course found. A model of this kind,involving transport by a dynamic membrane system, seems necessaryto explain the results. |
