Caruccio L, Bae S, Liu A Y, Chen K Y
Graduate Program in Biochemistry, Rutgers-The State University of New Jersey, Piscataway, NJ 08855-0939, USA.
Biochem J. 1997 Oct 15;327 ( Pt 2)(Pt 2):341-7. doi: 10.1042/bj3270341.
Osmoregulation, the cellular response to environmental changes of osmolarity and ionic strength, is important for the survival of living organisms. We have demonstrated previously that an exposure of mammalian cells to hypo-osmotic stress, either in growth medium (30% growth medium and 70% water) or in binary solution containing sorbitol and water, prominently induced the DNA-binding activity of the heat-shock transcription factor (HSF1) [Huang, Caruccio, Liu and Chen (1995) Biochem. J. 307, 347-352]. Since hyperosmotic and hypo-osmotic stress usually elicit opposite biological responses, we wondered what would be the effect of hyperosmotic stress on HSF activation. In this study we have examined the HSF DNA-binding activity in HeLa cells maintained in the sorbitol/water binary solution over a wide concentration range (0.1-0.9 M) and in Dulbecco's medium supplemented with sorbitol or NaCl. We found that HSF-binding activity could be induced prominently under both hypo-osmotic (0.1-0.25 M) and hyperosmotic conditions (0.50-0.90 M). In both cases, HSF activation was observed within 5 min after changing the osmotic pressure. The activation was accompanied by both HSF trimerization and nuclear translocation, and appeared to be independent of protein synthesis. The effects of hypo- or hyper-osmotic stress on HSF activation could be reversed once the cells were returned to iso-osmotic conditions (0.30M) with a half-life (t12) of 25 min or less. This rapid turnover of the osmotic-stress-induced HSF-binding activity was inhibited by cycloheximide, a potent inhibitor of protein synthesis. Unlike heat shock, activation of HSF by either hypo- or hyper-osmotic stress did not lead to an accumulation of heat-shock protein 70 (HSP70) mRNA in HeLa cells. We propose that HSF activation during osmotic stress may serve physiological functions independent of the synthesis of heat-shock proteins.
渗透调节,即细胞对渗透压和离子强度环境变化的反应,对生物体的生存至关重要。我们之前已经证明,将哺乳动物细胞暴露于低渗应激下,无论是在生长培养基(30%生长培养基和70%水)中,还是在含有山梨醇和水的二元溶液中,都会显著诱导热休克转录因子(HSF1)的DNA结合活性[黄、卡鲁乔、刘和陈(1995年)《生物化学杂志》307卷,347 - 352页]。由于高渗和低渗应激通常会引发相反的生物学反应,我们想知道高渗应激对HSF激活会有什么影响。在这项研究中,我们检测了在广泛浓度范围(0.1 - 0.9 M)的山梨醇/水二元溶液中以及添加了山梨醇或氯化钠的杜尔贝科培养基中培养的HeLa细胞中的HSF DNA结合活性。我们发现,在低渗(0.1 - 0.25 M)和高渗条件(0.50 - 0.90 M)下,HSF结合活性都能被显著诱导。在这两种情况下,改变渗透压后5分钟内就观察到了HSF激活。激活伴随着HSF三聚化和核转位,并且似乎与蛋白质合成无关。一旦细胞恢复到等渗条件(0.30M),低渗或高渗应激对HSF激活的影响可以在25分钟或更短的半衰期(t12)内逆转。这种由渗透压应激诱导的HSF结合活性的快速周转被蛋白质合成的强效抑制剂环己酰亚胺所抑制。与热休克不同,低渗或高渗应激激活HSF不会导致HeLa细胞中热休克蛋白70(HSP70)mRNA的积累。我们提出,渗透应激期间的HSF激活可能发挥独立于热休克蛋白合成的生理功能。