Natochin Iu V, Berger V Ia
Zh Evol Biokhim Fiziol. 1979 May-Jun;15(3):295-302.
Marine molluscs exhibit relative constancy in intracellular potassium at the back ground of significant changes in intracellular sodium during acclimation to differen salinities. These changes, which were observed in cells of the adductor muscle and hepa topancreas, result mainly from active extrusion of sodium (possibly, of chloride as well) from the cell at low salinities and accumulation of these ions within the cell during the increase in salinity. Changes in intracellular concentration of sodium and chloride ions serve presumably as one of the main mechanisms of volume stabilization of cells, which together with the amino acid regulation alleviates the hydration of cells at different salinities. The capacity of cells to keep their potassium accounts for the maintenance of Ki/Ko ratio during changes in cellular volume induced by osmotic effects. These data are discussed in relation to two alternative hypotheses of the decreased and close to the present salinity of ocean at the initial stages of formation of the ionic composition of cells.
在适应不同盐度的过程中,海洋软体动物细胞内钠含量发生显著变化,而细胞内钾含量则相对稳定。在内收肌和肝胰腺细胞中观察到的这些变化,主要是由于低盐度时细胞主动排出钠(可能还有氯),以及盐度升高时这些离子在细胞内积累所致。细胞内钠离子和氯离子浓度的变化可能是细胞体积稳定的主要机制之一,这与氨基酸调节共同作用,减轻了细胞在不同盐度下的水合作用。细胞保持钾的能力使得在渗透效应引起细胞体积变化期间,细胞内钾离子浓度与细胞外钾离子浓度之比(Ki/Ko)得以维持。结合细胞离子组成形成初期海洋盐度降低和接近当前盐度这两种相互替代的假说来讨论这些数据。