The marine archaebacterium Methanococcus jannaschii was studied at high temperatures and hyperbaric pressures of helium to investigate the effect of pressure on the behavior of a deep-sea thermophile. Methanogenesis and growth (as measured by protein production) at both 86 and 90°C were accelerated by pressure up to 750 atm (1 atm = 101.29kPa), but growth was not observed above 90°C at either 7.8 or 250 atm. However, growth and methanogenesis were uncoupled above 90°C, and the high-temperature limit for methanogenesis was increased by pressure. Substantial methane formation was evident at 98°C and 250 atm, whereas no methane formation was observed at 94°C and 7.8 atm. In contrast, when argon was substituted for helium as the pressurizing gas at 250 atm, no methane was produced at 86°C. Methanogenesis was also suppressed at 86°C and 250 atm when the culture was pressurized with a 4:1 mix of H 2 and CO 2 , although limited methanogenesis did occur when the culture was pressurized with H 2 .
CITATION STYLE
Miller, J. F., Shah, N. N., Nelson, C. M., Ludlow, J. M., & Clark, D. S. (1988). Pressure and Temperature Effects on Growth and Methane Production of the Extreme Thermophile Methanococcus jannaschii. Applied and Environmental Microbiology, 54(12), 3039–3042. https://doi.org/10.1128/aem.54.12.3039-3042.1988
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