Research Article 2339 Osmoregulation in Paramecium: in situ ion gradients permit water to cascade through the cytosol to the contractile vacuole Christian Stock1,*, Heidi K. Grønlien2, Richard D. Allen1 and Yutaka Naitoh1 1Pacific Biomedical Research Center, Snyder Hall 306, University of Hawaii at Manoa, 2538 The Mall, Honolulu, HI 96822, USA 2Department of Biology, University of Oslo, PO Box 1051, Blindern, N-0316 Oslo, Norway *Author for correspondence (e-mail:
[email protected]) Accepted 15 March 2002 Journal of Cell Science 115, 2339-2348 (2002) © The Company of Biologists Ltd Summary In vivo K+, Na+, Ca2+ and Cl– activities in the cytosol caused concomitant decreases in the cytosolic K+ and Cl– and the contractile vacuole fluid of Paramecium activities that were accompanied by a decrease in the water multimicronucleatum were determined in cells adapted to a segregation activity of the contractile vacuole complex. number of external osmolarities and ionic conditions by This implies that the cytosolic K+ and Cl– are actively co- using ion-selective microelectrodes. It was found that: (1) imported across the plasma membrane. Thus, the osmotic under standardized saline conditions K+ and Cl– were the gradients across both the plasma membrane and the major osmolytes in both the cytosol and the contractile membrane of the contractile vacuole complex ensure a vacuole fluid; and (2) the osmolarity of the contractile controlled cascade of water flow through the cell that can vacuole fluid, determined from K+ and Cl– activities only, provide for osmoregulation as well as the possible extrusion was always more than 1.5 times higher than that of the of metabolic waste by the contractile vacuole complex.