Variability of pressure adaptation in deep sea bacteria |
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Authors: | Holger W. Jannasch Carl O. Wirsen |
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Affiliation: | (1) Woods Hole Oceanographic Institution, 02543 Woods Hole, MA, USA |
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Abstract: | Isolations of pressure-adapted deep sea bacteria from depths of 1,400 to 5,100 m resulted in a variety of psychrophilic barotolerant and barophilic strains. Growth rates determined at different pressures indicated a gradual transition between the two types of pressure-adapted isolates. The presence of barotolerant bacteria in deep water, sustained by sinking particulate matter, causes the nonbarophilic response of natural populations, i.e., increased growth after decompression. With increasing pressure-adaptation in barophilic isolates the maximum growth rates at optimum pressures decrease. Thus, the observed general slow-down of microbial activity in the deep sea takes effect regardless of the common occurrence of psychrophilic and barophilic bacteria. The highest degree of barophilism was observed in isolates from nutrient-rich habitats such as intestinal tracts of deep sea animals or decaying carcasses. Detailed studies with an isolate, growing barophilically on a complex as well as a single-carbon-source medium, showed that (1) culturing at pressures lower than optimal for growth resulted in the formation of cell filaments, (2) growth was unaffected by repeated compression/decompression cycles and (3) no perceptible differences in the distribution of radiolabeled carbon from an amino acid mixture occurred in cells grown at, below and above the pressure optimal for growth.Dedicated to Professor Dr. Hans G. Schlegel on the occasion of his 60th birthday in recognition of his broad microbiological interests and in special appreciation of his lasting support for the Marine Microbiology Course at the Stazione Zoologica (Naples, Italy) now for almost 25 yearsNon-standard abbreviations. The traditional use of atm as a unit of pressure (=10 m of water column, =1.013 bar, =101.3 kN/m2) is retained here in view of the important relation between water depth and hydrostatic pressure in the present study. Due to the compression of seawater and the geographic variability of gravity, there is a progressive deviation of the actual pressure with depth amounting to +4.9 atm at 5,000 m and a latitude of 30°. EPC, cell counts obtained by epifluorescence microscopy. PY, peptone yeast extract medium |
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Keywords: | Marine bacteria Deep sea Barotolerance Barophilism Pressure adaptation Psychrophilism |
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