Are thermophilic microorganisms active in cold environments?
Abstract 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 albed...
Published in: | International Journal of Astrobiology |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
2014
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Subjects: | |
Online Access: | https://doi.org/10.1017/s1473550414000433 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S1473550414000433 |
_version_ | 1831201208724881408 |
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author | Cockell, Charles S. Cousins, Claire Wilkinson, Paul T. Olsson-Francis, Karen Rozitis, Ben |
author_facet | Cockell, Charles S. Cousins, Claire Wilkinson, Paul T. Olsson-Francis, Karen Rozitis, Ben |
author_sort | Cockell, Charles S. |
collection | Cambridge University Press |
container_issue | 3 |
container_start_page | 457 |
container_title | International Journal of Astrobiology |
container_volume | 14 |
description | Abstract 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. |
format | Article in Journal/Newspaper |
genre | Iceland |
genre_facet | Iceland |
id | crcambridgeupr:10.1017/s1473550414000433 |
institution | Open Polar |
language | English |
op_collection_id | crcambridgeupr |
op_container_end_page | 463 |
op_doi | https://doi.org/10.1017/s1473550414000433 |
op_rights | https://www.cambridge.org/core/terms |
op_source | International Journal of Astrobiology volume 14, issue 3, page 457-463 ISSN 1473-5504 1475-3006 |
publishDate | 2014 |
publisher | Cambridge University Press (CUP) |
record_format | openpolar |
spelling | crcambridgeupr:10.1017/s1473550414000433 2025-05-04T14:28:34+00:00 Are thermophilic microorganisms active in cold environments? Cockell, Charles S. Cousins, Claire Wilkinson, Paul T. Olsson-Francis, Karen Rozitis, Ben 2014 https://doi.org/10.1017/s1473550414000433 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S1473550414000433 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms International Journal of Astrobiology volume 14, issue 3, page 457-463 ISSN 1473-5504 1475-3006 journal-article 2014 crcambridgeupr https://doi.org/10.1017/s1473550414000433 2025-04-08T13:31:13Z Abstract 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. Article in Journal/Newspaper Iceland Cambridge University Press International Journal of Astrobiology 14 3 457 463 |
spellingShingle | Cockell, Charles S. Cousins, Claire Wilkinson, Paul T. Olsson-Francis, Karen Rozitis, Ben Are thermophilic microorganisms active in cold environments? |
title | Are thermophilic microorganisms active in cold environments? |
title_full | Are thermophilic microorganisms active in cold environments? |
title_fullStr | Are thermophilic microorganisms active in cold environments? |
title_full_unstemmed | Are thermophilic microorganisms active in cold environments? |
title_short | Are thermophilic microorganisms active in cold environments? |
title_sort | are thermophilic microorganisms active in cold environments? |
url | https://doi.org/10.1017/s1473550414000433 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S1473550414000433 |