Are thermophilic microorganisms active in cold environments?

The authors thank the STFC for providing a studentship to PW for this work. This work was made possible with support from the UK Science and Technology Facilities Council (STFC; Grant No. ST/1001964/1). The mean air temperature of the Icelandic interior is below 10 °C. However, we have previously ob...

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Bibliographic Details
Published in:International Journal of Astrobiology
Main Authors: Cockell, Charles S., Cousins, Claire Rachel, Wilkinson, Paul T., Olsson-Francis, Karen, Rozitis, Ben
Other Authors: University of St Andrews.Earth and Environmental Sciences
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Thermophiles
Extremophiles
Volcanic
Mars
Geomicrobiology
GE Environmental Sciences
QC Physics
QB Astronomy
NDAS
GE
QC
QB
Iceland
Online Access:https://hdl.handle.net/10023/10885
https://doi.org/10.1017/S1473550414000433
Description
Summary:The authors thank the STFC for providing a studentship to PW for this work. This work was made possible with support from the UK Science and Technology Facilities Council (STFC; Grant No. ST/1001964/1). The mean air temperature of the Icelandic interior is below 10 °C. However, we have previously observed 16S rDNA sequences associated with thermophilic lineages in Icelandic basalts. Measurements of the temperatures of igneous rocks in Iceland showed that solar insolation of these low albedo substrates achieved a peak surface temperature of 44.5 °C. We isolated seven thermophilic Geobacillus species from basalt with optimal growth temperatures of ~65 °C. The minimum growth temperature of these organisms was ~36 °C, suggesting that they could be active in the rock environment. Basalt dissolution rates at 40 °C were increased in the presence of one of the isolates compared to abiotic controls, showing its potential to be involved in active biogeochemistry at environmental temperatures. These data raise the possibility of transient active thermophilic growth in macroclimatically cold rocky environments, implying that the biogeographical distribution of active thermophiles might be greater than previously understood. These data show that temperatures measured or predicted over large scales on a planet are not in themselves adequate to assess niches available to extremophiles at micron scales. Peer reviewed

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