Heterotrophic and Autotrophic Microbial Populations in Cold Perennial Springs of the High Arctic ▿ †
The saline springs of Gypsum Hill in the Canadian high Arctic are a rare example of cold springs originating from deep groundwater and rising to the surface through thick permafrost. The heterotrophic bacteria and autotrophic sulfur-oxidizing bacteria (up to 40% of the total microbial community) iso...
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ftpubmed:oai:pubmedcentral.nih.gov:2583501 2023-05-15T14:53:32+02:00 Heterotrophic and Autotrophic Microbial Populations in Cold Perennial Springs of the High Arctic ▿ † Perreault, Nancy N. Greer, Charles W. Andersen, Dale T. Tille, Stefanie Lacrampe-Couloume, Georges Lollar, Barbara Sherwood Whyte, Lyle G. 2008-11 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2583501 http://www.ncbi.nlm.nih.gov/pubmed/18805995 https://doi.org/10.1128/AEM.00359-08 en eng American Society for Microbiology (ASM) http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2583501 http://www.ncbi.nlm.nih.gov/pubmed/18805995 http://dx.doi.org/10.1128/AEM.00359-08 Copyright © 2008, American Society for Microbiology Microbial Ecology Text 2008 ftpubmed https://doi.org/10.1128/AEM.00359-08 2013-09-02T07:50:04Z The saline springs of Gypsum Hill in the Canadian high Arctic are a rare example of cold springs originating from deep groundwater and rising to the surface through thick permafrost. The heterotrophic bacteria and autotrophic sulfur-oxidizing bacteria (up to 40% of the total microbial community) isolated from the spring waters and sediments were classified into four phyla (Actinobacteria, Bacteroidetes, Firmicutes, and Proteobacteria) based on 16S rRNA gene analysis; heterotrophic isolates were primarily psychrotolerant, salt-tolerant, facultative anaerobes. Some of the isolates contained genes for thiosulfate oxidation (soxB) and anoxygenic photosynthesis (pufM), possibly enabling the strains to better compete in these sulfur-rich environments subject to long periods of illumination in the Arctic summer. Although leucine uptake by the spring water microbial community was low, CO2 uptake was relatively high under dark incubation, reinforcing the idea that primary production by chemoautotrophs is an important process in the springs. The small amounts of hydrocarbons in gases exsolving from the springs (0.38 to 0.51% CH4) were compositionally and isotopically consistent with microbial methanogenesis and possible methanotrophy. Anaerobic heterotrophic sulfur oxidation and aerobic autotrophic sulfur oxidation activities were demonstrated in sediment slurries. Overall, our results describe an active microbial community capable of sustainability in an extreme environment that experiences prolonged periods of continuous light or darkness, low temperatures, and moderate salinity, where life seems to rely on chemolithoautotrophy. Text Arctic permafrost PubMed Central (PMC) Arctic Gypsum Hill ENVELOPE(-90.751,-90.751,79.402,79.402) Applied and Environmental Microbiology 74 22 6898 6907 |
institution |
Open Polar |
collection |
PubMed Central (PMC) |
op_collection_id |
ftpubmed |
language |
English |
topic |
Microbial Ecology |
spellingShingle |
Microbial Ecology Perreault, Nancy N. Greer, Charles W. Andersen, Dale T. Tille, Stefanie Lacrampe-Couloume, Georges Lollar, Barbara Sherwood Whyte, Lyle G. Heterotrophic and Autotrophic Microbial Populations in Cold Perennial Springs of the High Arctic ▿ † |
topic_facet |
Microbial Ecology |
description |
The saline springs of Gypsum Hill in the Canadian high Arctic are a rare example of cold springs originating from deep groundwater and rising to the surface through thick permafrost. The heterotrophic bacteria and autotrophic sulfur-oxidizing bacteria (up to 40% of the total microbial community) isolated from the spring waters and sediments were classified into four phyla (Actinobacteria, Bacteroidetes, Firmicutes, and Proteobacteria) based on 16S rRNA gene analysis; heterotrophic isolates were primarily psychrotolerant, salt-tolerant, facultative anaerobes. Some of the isolates contained genes for thiosulfate oxidation (soxB) and anoxygenic photosynthesis (pufM), possibly enabling the strains to better compete in these sulfur-rich environments subject to long periods of illumination in the Arctic summer. Although leucine uptake by the spring water microbial community was low, CO2 uptake was relatively high under dark incubation, reinforcing the idea that primary production by chemoautotrophs is an important process in the springs. The small amounts of hydrocarbons in gases exsolving from the springs (0.38 to 0.51% CH4) were compositionally and isotopically consistent with microbial methanogenesis and possible methanotrophy. Anaerobic heterotrophic sulfur oxidation and aerobic autotrophic sulfur oxidation activities were demonstrated in sediment slurries. Overall, our results describe an active microbial community capable of sustainability in an extreme environment that experiences prolonged periods of continuous light or darkness, low temperatures, and moderate salinity, where life seems to rely on chemolithoautotrophy. |
format |
Text |
author |
Perreault, Nancy N. Greer, Charles W. Andersen, Dale T. Tille, Stefanie Lacrampe-Couloume, Georges Lollar, Barbara Sherwood Whyte, Lyle G. |
author_facet |
Perreault, Nancy N. Greer, Charles W. Andersen, Dale T. Tille, Stefanie Lacrampe-Couloume, Georges Lollar, Barbara Sherwood Whyte, Lyle G. |
author_sort |
Perreault, Nancy N. |
title |
Heterotrophic and Autotrophic Microbial Populations in Cold Perennial Springs of the High Arctic ▿ † |
title_short |
Heterotrophic and Autotrophic Microbial Populations in Cold Perennial Springs of the High Arctic ▿ † |
title_full |
Heterotrophic and Autotrophic Microbial Populations in Cold Perennial Springs of the High Arctic ▿ † |
title_fullStr |
Heterotrophic and Autotrophic Microbial Populations in Cold Perennial Springs of the High Arctic ▿ † |
title_full_unstemmed |
Heterotrophic and Autotrophic Microbial Populations in Cold Perennial Springs of the High Arctic ▿ † |
title_sort |
heterotrophic and autotrophic microbial populations in cold perennial springs of the high arctic ▿ † |
publisher |
American Society for Microbiology (ASM) |
publishDate |
2008 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2583501 http://www.ncbi.nlm.nih.gov/pubmed/18805995 https://doi.org/10.1128/AEM.00359-08 |
long_lat |
ENVELOPE(-90.751,-90.751,79.402,79.402) |
geographic |
Arctic Gypsum Hill |
geographic_facet |
Arctic Gypsum Hill |
genre |
Arctic permafrost |
genre_facet |
Arctic permafrost |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC2583501 http://www.ncbi.nlm.nih.gov/pubmed/18805995 http://dx.doi.org/10.1128/AEM.00359-08 |
op_rights |
Copyright © 2008, American Society for Microbiology |
op_doi |
https://doi.org/10.1128/AEM.00359-08 |
container_title |
Applied and Environmental Microbiology |
container_volume |
74 |
container_issue |
22 |
container_start_page |
6898 |
op_container_end_page |
6907 |
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1766325118668111872 |