Heat resistance of bacterial spores correlated with protoplast dehydration, mineralization, and thermal adaptation.
Twenty-eight types of lysozyme-sensitive spores among seven Bacillus species representative of thermophiles, mesophiles, and psychrophiles were obtained spanning a 3,000-fold range in moist-heat resistance. The resistance within species was altered by demineralization of the native spores to protonated spores and remineralization of the protonated spores to calcified spores and by thermal adaptation at maximum, optimum, and minimum sporulation temperatures. Protoplast wet densities, and thereby protoplast water contents, were obtained by buoyant density sedimentation in Nycodenz gradients (Nyegaard and Co., Oslo, Norway). Increases in mineralization and thermal adaptation caused reductions in protoplast water content between limits of ca. 57 and 28% (wet weight basis), and thereby correlated with increases in sporal heat resistance. Above and below these limits, however, increases in mineralization and thermal adaptation correlated with increases in sporal resistance independently of unchanged protoplast water contents. All three factors evidently contributed to and were necessary for heat resistance of the spores, but dehydration predominated.
D000222:Adaptation, Physiological; D001407:Bacillus / Q000502:physiology*; D001409:Bacillus cereus / Q000502:physiology; D002113:Calcification, Physiologic; D003890:Desiccation; D001411:Geobacillus stearothermophilus / Q000502:physiology; D006358:Hot Temperature; D011523:Protoplasts / Q000502:physiology; D013171:Spores, Bacterial / Q000502:physiology