Iwamoto Masaaki, Sugino Kazuyuki, Allen Richard D, Naitoh Yutaka
Pacific Biomedical Research Center, Snyder Hall 306, University of Hawaii at Manoa, 2538 The Mall, Honolulu, HI 96822, USA.
J Exp Biol. 2005 Feb;208(Pt 3):523-37. doi: 10.1242/jeb.01417.
A fresh water protozoan Paramecium multimicronucleatum adapted to a given solution was found to swell until the osmotic pressure difference between the cytosol and the solution balanced the cytosolic pressure. The cytosolic pressure was generated as the cell swelled osmotically. When either one or both of these pressures was somehow modified, cell volume would change until a new balance between these pressures was established. A hypothetical osmolyte transport mechanism(s) was presumably activated when the cytosolic pressure exceeded the threshold value of approximately 1.5 x 10(5) Pa as the cell swelled after its subjection to a decreased osmolarity. The cytosolic osmolarity thereby decreased and the volume of the swollen cell resumed its initial value. This corresponds to regulatory volume decrease (RVD). By contrast, another hypothetical osmolyte transport mechanism(s) was activated when the cell shrank after its subjection to an increased osmolarity. The cytosolic osmolarity thereby increased and volume of the shrunken cell resumed its initial value. This corresponds to regulatory volume increase (RVI). The osmolyte transport mechanism responsible for RVD might be activated again when the external osmolarity decreases further, and the cytosolic osmolarity thereby decreases to the next lower level. Similarly, another osmolyte transport mechanism responsible for RVI might be activated again when the external osmolarity increases further, and the cytosolic osmolarity thereby increases to the next higher level. Stepwise changes in the cytosolic osmolarity caused by a gradual change in the adaptation osmolarity found in P. multimicronucleatum is attributable to these osmolyte transport mechanisms. An abrupt change in the amount of fluid discharged from the contractile vacuole seen immediately after changing the external osmolarity reduces an abrupt change in cell volume and thereby protects the cell from the disruption of the plasma membrane by excessive stretch or dehydration during shrinkage.
研究发现,一种适应特定溶液的淡水原生动物多核草履虫会膨胀,直至细胞质与溶液之间的渗透压差异平衡细胞质压力。细胞质压力是细胞通过渗透作用膨胀时产生的。当这两种压力中的任何一种或两种以某种方式改变时,细胞体积就会发生变化,直到这些压力之间建立新的平衡。当细胞在渗透压降低后膨胀,细胞质压力超过约1.5×10⁵帕的阈值时,推测一种假设的渗透溶质转运机制被激活。细胞质渗透压由此降低,膨胀细胞的体积恢复到初始值。这对应于调节性体积减小(RVD)。相比之下,当细胞在渗透压升高后收缩时,另一种假设的渗透溶质转运机制被激活。细胞质渗透压由此升高,收缩细胞的体积恢复到初始值。这对应于调节性体积增大(RVI)。当外部渗透压进一步降低,细胞质渗透压随之降至下一个更低水平时,负责RVD的渗透溶质转运机制可能会再次被激活。同样,当外部渗透压进一步升高,细胞质渗透压随之升至下一个更高水平时,另一种负责RVI的渗透溶质转运机制可能会再次被激活。多核草履虫中适应渗透压的逐渐变化导致细胞质渗透压的逐步变化,这归因于这些渗透溶质转运机制。在改变外部渗透压后立即观察到的收缩泡排出液体量的突然变化,减少了细胞体积的突然变化,从而保护细胞在收缩过程中免受过度拉伸或脱水导致的质膜破裂。