Survival of Desulfotomaculum spores from estuarine sediments after serial autoclaving and high-temperature exposureReport as inadecuate




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1 School of Earth and Ocean Sciences Cardiff 2 Cardiff School of Biosciences 3 School of Civil Engineering & Geosciences Newcastle

Abstract : Bacterial spores are widespread in marine sediments, including those of thermophilic, sulphate-reducing bacteria, which have a high minimum growth temperature making it unlikely that they grow in situ. These Desulfotomaculum spp. are thought to be from hot environments and are distributed by ocean currents. Their cells and spores upper temperature limit for survival is unknown, as is whether they can survive repeated high-temperature exposure that might occur in hydrothermal systems. This was investigated by incubating estuarine sediments significantly above 40–80 1C maximum in situ temperatures B23 1C, and with and without prior triple autoclaving. Sulphate reduction occurred at 40–60 1C and at 60 1C was unaffected by autoclaving. Desulfotomaculum sp. C1A60 was isolated and was most closely related to the thermophilic D. kuznetsovii T B96% 16S rRNA gene sequence identity. Cultures of Desulfotomaculum sp. C1A60, D. kuznetsovii T and D. geothermicum B2T survived triple autoclaving while other related Desulfotomaculum spp. did not, although they did survive pasteurisation. Desulfotomaculum sp. C1A60 and D. kuznetsovii cultures also survived more extreme autoclaving C1A60, 130 1C for 15 min; D. kuznetsovii, 135 1C for 15 min, maximum of 154 1C reached and high-temperature conditions in an oil bath C1A60, 1301 for 30 min, D. kuznetsovii 140 1C for 15 min. Desulfotomaculum sp. C1A60 with either spores or predominantly vegetative cells demonstrated that surviving triple autoclaving was due to spores. Spores also had very high culturability compared with vegetative cells B30 Â higher. Combined extreme temperature survival and high culturability of some thermophilic Desulfotomaculum spp. make them very effective colonisers of hot environments, which is consistent with their presence in subsurface geothermal waters and petroleum reservoirs.





Author: Louise A. O’sullivan - Erwan Roussel - Andrew J. Weightman - Gordon Webster - Casey R. J. Hubert - Emma Bell - Ian Head - Henri

Source: https://hal.archives-ouvertes.fr/



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