Distinct Bacterial Communities Exist beneath a High Arctic Polythermal Glacier
ABSTRACT Bacterial communities reside in basal ice, sediment, and meltwater in the supra-, sub-, and proglacial environments of John Evans Glacier, Nunavut, Canada. We examined whether the subglacial bacterial community shares common members with the pro- and supraglacial communities, and by inferen...
Published in: | Applied and Environmental Microbiology |
---|---|
Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Society for Microbiology
2006
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1128/aem.00595-06 https://journals.asm.org/doi/pdf/10.1128/AEM.00595-06 |
id |
crasmicro:10.1128/aem.00595-06 |
---|---|
record_format |
openpolar |
spelling |
crasmicro:10.1128/aem.00595-06 2024-09-15T18:08:01+00:00 Distinct Bacterial Communities Exist beneath a High Arctic Polythermal Glacier Bhatia, Maya Sharp, Martin Foght, Julia 2006 http://dx.doi.org/10.1128/aem.00595-06 https://journals.asm.org/doi/pdf/10.1128/AEM.00595-06 en eng American Society for Microbiology https://journals.asm.org/non-commercial-tdm-license Applied and Environmental Microbiology volume 72, issue 9, page 5838-5845 ISSN 0099-2240 1098-5336 journal-article 2006 crasmicro https://doi.org/10.1128/aem.00595-06 2024-08-26T04:06:26Z ABSTRACT Bacterial communities reside in basal ice, sediment, and meltwater in the supra-, sub-, and proglacial environments of John Evans Glacier, Nunavut, Canada. We examined whether the subglacial bacterial community shares common members with the pro- and supraglacial communities, and by inference, whether it could be derived from communities in either of these environments (e.g., by ice overriding proglacial sediments or by in-wash of surface meltwaters). Terminal restriction fragment length polymorphism analysis of bacterial 16S rRNA genes amplified from these environments revealed that the subglacial water, basal ice, and sediment communities were distinct from those detected in supraglacial meltwater and proglacial sediments, with 60 of 142 unique terminal restriction fragments (T-RFs) detected exclusively in subglacial samples and only 8 T-RFs detected in all three environments. Supraglacial waters shared some T-RFs with subglacial water and ice, likely reflecting the seasonal flow of surface meltwater into the subglacial drainage system, whereas supraglacial and proglacial communities shared the fewest T-RFs. Thus, the subglacial community at John Evans Glacier appears to be predominantly autochthonous rather than allochthonous, and it may be adapted to subglacial conditions. Chemical analysis of water and melted ice also revealed differences between the supraglacial and proglacial environments, particularly regarding electrical conductivity and nitrate, sulfate, and dissolved organic carbon concentrations. Whereas the potential exists for common bacterial types to be broadly distributed throughout the glacial system, we have observed distinct bacterial communities in physically and chemically different glacial environments. Article in Journal/Newspaper glacier* Nunavut ASM Journals (American Society for Microbiology) Applied and Environmental Microbiology 72 9 5838 5845 |
institution |
Open Polar |
collection |
ASM Journals (American Society for Microbiology) |
op_collection_id |
crasmicro |
language |
English |
description |
ABSTRACT Bacterial communities reside in basal ice, sediment, and meltwater in the supra-, sub-, and proglacial environments of John Evans Glacier, Nunavut, Canada. We examined whether the subglacial bacterial community shares common members with the pro- and supraglacial communities, and by inference, whether it could be derived from communities in either of these environments (e.g., by ice overriding proglacial sediments or by in-wash of surface meltwaters). Terminal restriction fragment length polymorphism analysis of bacterial 16S rRNA genes amplified from these environments revealed that the subglacial water, basal ice, and sediment communities were distinct from those detected in supraglacial meltwater and proglacial sediments, with 60 of 142 unique terminal restriction fragments (T-RFs) detected exclusively in subglacial samples and only 8 T-RFs detected in all three environments. Supraglacial waters shared some T-RFs with subglacial water and ice, likely reflecting the seasonal flow of surface meltwater into the subglacial drainage system, whereas supraglacial and proglacial communities shared the fewest T-RFs. Thus, the subglacial community at John Evans Glacier appears to be predominantly autochthonous rather than allochthonous, and it may be adapted to subglacial conditions. Chemical analysis of water and melted ice also revealed differences between the supraglacial and proglacial environments, particularly regarding electrical conductivity and nitrate, sulfate, and dissolved organic carbon concentrations. Whereas the potential exists for common bacterial types to be broadly distributed throughout the glacial system, we have observed distinct bacterial communities in physically and chemically different glacial environments. |
format |
Article in Journal/Newspaper |
author |
Bhatia, Maya Sharp, Martin Foght, Julia |
spellingShingle |
Bhatia, Maya Sharp, Martin Foght, Julia Distinct Bacterial Communities Exist beneath a High Arctic Polythermal Glacier |
author_facet |
Bhatia, Maya Sharp, Martin Foght, Julia |
author_sort |
Bhatia, Maya |
title |
Distinct Bacterial Communities Exist beneath a High Arctic Polythermal Glacier |
title_short |
Distinct Bacterial Communities Exist beneath a High Arctic Polythermal Glacier |
title_full |
Distinct Bacterial Communities Exist beneath a High Arctic Polythermal Glacier |
title_fullStr |
Distinct Bacterial Communities Exist beneath a High Arctic Polythermal Glacier |
title_full_unstemmed |
Distinct Bacterial Communities Exist beneath a High Arctic Polythermal Glacier |
title_sort |
distinct bacterial communities exist beneath a high arctic polythermal glacier |
publisher |
American Society for Microbiology |
publishDate |
2006 |
url |
http://dx.doi.org/10.1128/aem.00595-06 https://journals.asm.org/doi/pdf/10.1128/AEM.00595-06 |
genre |
glacier* Nunavut |
genre_facet |
glacier* Nunavut |
op_source |
Applied and Environmental Microbiology volume 72, issue 9, page 5838-5845 ISSN 0099-2240 1098-5336 |
op_rights |
https://journals.asm.org/non-commercial-tdm-license |
op_doi |
https://doi.org/10.1128/aem.00595-06 |
container_title |
Applied and Environmental Microbiology |
container_volume |
72 |
container_issue |
9 |
container_start_page |
5838 |
op_container_end_page |
5845 |
_version_ |
1810445367997628416 |