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Osmotic adjustment in marine yeast
Authors:Hernandez-Saavedra  Norma Y; Ochoa  Jose Luis; Vazquez-Dulhalt  Rafael
Institution:Center for Biological Research PO Box 128, La Paz, Baja California Sur, 23000 Mexico 1Department of Microbiology, University of Alberta Edmonton, Alberta, T6G 2E9, Canada
Abstract:The effect of environmental salinity on cell growth, and onthe composition and accumulation of compatible solutes, or osmotica,of five yeast strains (Aureobasidium pullulans, Candida sp.,Cryptococcus albidus var. albidus, Debaryomyces hansenii andRhodotorula rubra) was compared. All these yeast were isolatedfrom manne environments, but were able to grow in the absenceof salt and should therefore be considered as halotolerant strains.According to their specific cell growth rates at different saltconcentrations, these strains vary in their capacity to osmoticallyadjust to modifications in external salinity. Candida sp. appearsto be the most sensitive since the maximum salt concentrationat which it can grow is 1.54 mol 1-1 NaCl; however, it showedthe highest specific cell growth in the range of 0 to 1.54 mol1-1 NaCl. Aureobasidium pullulans, on the other hand, showedthe lowest specific growth rate, but the highest halotolerancerange from 0 to 5.13 mol 1-1 NaCl. Debaryomyces hansenii, incontrast, showed higher specific growth at this salinity rangeCryptococcus albidus var. albidus and Rhodotorula rubra showedsimilar specific cell growth rate values and halotolerance between0 and 2.45 mol 1-1 NaCl. The protein and carbohydrate contentof the biomass of the different yeast cells, as a result ofexternal salinity vanation, remained practically constant. Themost important effects of the increase in salt concentrationin the culture medium were the reduction of cell volume andthe accumulation of low-molecular-weight metabolites (LMWM).which appear to act as osmoregulators. Glycerol was found asthe major compatible solute in the different marine yeasts studiedherein with a total contribution of 64–96% of the internalcell osmolarity. Other LMWM, like carbohydrates and amino acids,contributed to a lesser extent to compensate for the rise inosmotic pressure promoted by the salinity of the external environment.
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