Defining the functional potential and active community members of a sediment microbial community in a high-arctic hypersaline subzero spring

The Lost Hammer (LH) Spring is the coldest and saltiest terrestrial spring discovered to date and is characterized by perennial discharges at subzero temperatures (-5°C), hypersalinity (salinity, 24%), and reducing (≈-165mV), microoxic, and oligotrophic conditions. It is rich in sulfates (10.0%, wt/...

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Published in:Applied and Environmental Microbiology
Main Authors: Lay, C.-Y., Mykytczuk, N.C.S., Yergeau, É., Lamarche-Gagnon, G., Greer, C.W., Whyte, L.G.
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
RNA
DNA
16S
Online Access:https://doi.org/10.1128/AEM.00153-13
https://nrc-publications.canada.ca/eng/view/object/?id=10066444-a0de-4d4f-8826-203bb06c265a
https://nrc-publications.canada.ca/fra/voir/objet/?id=10066444-a0de-4d4f-8826-203bb06c265a
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spelling ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:21269891 2023-05-15T14:55:22+02:00 Defining the functional potential and active community members of a sediment microbial community in a high-arctic hypersaline subzero spring Lay, C.-Y. Mykytczuk, N.C.S. Yergeau, É. Lamarche-Gagnon, G. Greer, C.W. Whyte, L.G. 2013 text https://doi.org/10.1128/AEM.00153-13 https://nrc-publications.canada.ca/eng/view/object/?id=10066444-a0de-4d4f-8826-203bb06c265a https://nrc-publications.canada.ca/fra/voir/objet/?id=10066444-a0de-4d4f-8826-203bb06c265a eng eng issn:0099-2240 Applied and Environmental Microbiology, Volume: 79, Issue: 12, Publication date: 2013, Pages: 3637–3648 doi:10.1128/AEM.00153-13 Metagenomic analysis Microbial communities Microbial components Microbial populations Oligotrophic conditions Permafrost environment Stress response genes Sub-zero temperatures Ammonia Genes Metabolism Methane Microorganisms RNA Sulfur Sulfur compounds complementary DNA primer DNA RNA 16S adaptation discharge environmental stress enzyme activity fluvial deposit genetic analysis hypersaline environment microbial community nutrient cycling oxidation population structure terrestrial ecosystem archaeon Arctic Bacteroidetes cold cyanobacterium DNA sequence genetics metagenome microbiology molecular genetics natural spring nucleotide sequence Proteobacteria salinity sediment Archaea Arctic Regions Base Sequence Cold Temperature Cyanobacteria DNA Primers DNA Complementary Geologic Sediments Molecular Sequence Data Natural Springs Ribosomal 16S Sequence Analysis Canada article 2013 ftnrccanada https://doi.org/10.1128/AEM.00153-13 2021-09-01T06:27:49Z The Lost Hammer (LH) Spring is the coldest and saltiest terrestrial spring discovered to date and is characterized by perennial discharges at subzero temperatures (-5°C), hypersalinity (salinity, 24%), and reducing (≈-165mV), microoxic, and oligotrophic conditions. It is rich in sulfates (10.0%, wt/wt), dissolved H2S/sulfides (up to 25ppm), ammonia (≈381μM), and methane (11.1g day-1). To determine its total functional and genetic potential and to identify its active microbial components, we performed metagenomic analyses of the LH Spring outlet microbial community and pyrosequencing analyses of the cDNA of its 16S rRNA genes. Reads related to Cyanobacteria (19.7%), Bacteroidetes (13.3%), and Proteobacteria (6.6%) represented the dominant phyla identified among the classified sequences. Reconstruction of the enzyme pathways responsible for bacterial nitrification/ denitrification/ammonification and sulfate reduction appeared nearly complete in the metagenomic data set. In the cDNA profile of the LH Spring active community, ammonia oxidizers (Thaumarchaeota), denitrifiers (Pseudomonas spp.), sulfate reducers (Desulfobulbus spp.), and other sulfur oxidizers (Thermoprotei) were present, highlighting their involvement in nitrogen and sulfur cycling. Stress response genes for adapting to cold, osmotic stress, and oxidative stress were also abundant in the metagenome. Comparison of the composition of the functional community of the LH Spring to metagenomes from other saline/ subzero environments revealed a close association between the LH Spring and another Canadian high-Arctic permafrost environment, particularly in genes related to sulfur metabolism and dormancy. Overall, this study provides insights into the metabolic potential and the active microbial populations that exist in this hypersaline cryoenvironment and contributes to our understanding of microbial ecology in extreme environments. © 2013, American Society for Microbiology. Peer reviewed: Yes NRC publication: Yes Article in Journal/Newspaper Arctic permafrost National Research Council Canada: NRC Publications Archive Arctic Canada Applied and Environmental Microbiology 79 12 3637 3648
institution Open Polar
collection National Research Council Canada: NRC Publications Archive
op_collection_id ftnrccanada
language English
topic Metagenomic analysis
Microbial communities
Microbial components
Microbial populations
Oligotrophic conditions
Permafrost environment
Stress response genes
Sub-zero temperatures
Ammonia
Genes
Metabolism
Methane
Microorganisms
RNA
Sulfur
Sulfur compounds
complementary DNA
primer DNA
RNA 16S
adaptation
discharge
environmental stress
enzyme activity
fluvial deposit
genetic analysis
hypersaline environment
microbial community
nutrient cycling
oxidation
population structure
terrestrial ecosystem
archaeon
Arctic
Bacteroidetes
cold
cyanobacterium
DNA sequence
genetics
metagenome
microbiology
molecular genetics
natural spring
nucleotide sequence
Proteobacteria
salinity
sediment
Archaea
Arctic Regions
Base Sequence
Cold Temperature
Cyanobacteria
DNA Primers
DNA
Complementary
Geologic Sediments
Molecular Sequence Data
Natural Springs
Ribosomal
16S
Sequence Analysis
Canada
spellingShingle Metagenomic analysis
Microbial communities
Microbial components
Microbial populations
Oligotrophic conditions
Permafrost environment
Stress response genes
Sub-zero temperatures
Ammonia
Genes
Metabolism
Methane
Microorganisms
RNA
Sulfur
Sulfur compounds
complementary DNA
primer DNA
RNA 16S
adaptation
discharge
environmental stress
enzyme activity
fluvial deposit
genetic analysis
hypersaline environment
microbial community
nutrient cycling
oxidation
population structure
terrestrial ecosystem
archaeon
Arctic
Bacteroidetes
cold
cyanobacterium
DNA sequence
genetics
metagenome
microbiology
molecular genetics
natural spring
nucleotide sequence
Proteobacteria
salinity
sediment
Archaea
Arctic Regions
Base Sequence
Cold Temperature
Cyanobacteria
DNA Primers
DNA
Complementary
Geologic Sediments
Molecular Sequence Data
Natural Springs
Ribosomal
16S
Sequence Analysis
Canada
Lay, C.-Y.
Mykytczuk, N.C.S.
Yergeau, É.
Lamarche-Gagnon, G.
Greer, C.W.
Whyte, L.G.
Defining the functional potential and active community members of a sediment microbial community in a high-arctic hypersaline subzero spring
topic_facet Metagenomic analysis
Microbial communities
Microbial components
Microbial populations
Oligotrophic conditions
Permafrost environment
Stress response genes
Sub-zero temperatures
Ammonia
Genes
Metabolism
Methane
Microorganisms
RNA
Sulfur
Sulfur compounds
complementary DNA
primer DNA
RNA 16S
adaptation
discharge
environmental stress
enzyme activity
fluvial deposit
genetic analysis
hypersaline environment
microbial community
nutrient cycling
oxidation
population structure
terrestrial ecosystem
archaeon
Arctic
Bacteroidetes
cold
cyanobacterium
DNA sequence
genetics
metagenome
microbiology
molecular genetics
natural spring
nucleotide sequence
Proteobacteria
salinity
sediment
Archaea
Arctic Regions
Base Sequence
Cold Temperature
Cyanobacteria
DNA Primers
DNA
Complementary
Geologic Sediments
Molecular Sequence Data
Natural Springs
Ribosomal
16S
Sequence Analysis
Canada
description The Lost Hammer (LH) Spring is the coldest and saltiest terrestrial spring discovered to date and is characterized by perennial discharges at subzero temperatures (-5°C), hypersalinity (salinity, 24%), and reducing (≈-165mV), microoxic, and oligotrophic conditions. It is rich in sulfates (10.0%, wt/wt), dissolved H2S/sulfides (up to 25ppm), ammonia (≈381μM), and methane (11.1g day-1). To determine its total functional and genetic potential and to identify its active microbial components, we performed metagenomic analyses of the LH Spring outlet microbial community and pyrosequencing analyses of the cDNA of its 16S rRNA genes. Reads related to Cyanobacteria (19.7%), Bacteroidetes (13.3%), and Proteobacteria (6.6%) represented the dominant phyla identified among the classified sequences. Reconstruction of the enzyme pathways responsible for bacterial nitrification/ denitrification/ammonification and sulfate reduction appeared nearly complete in the metagenomic data set. In the cDNA profile of the LH Spring active community, ammonia oxidizers (Thaumarchaeota), denitrifiers (Pseudomonas spp.), sulfate reducers (Desulfobulbus spp.), and other sulfur oxidizers (Thermoprotei) were present, highlighting their involvement in nitrogen and sulfur cycling. Stress response genes for adapting to cold, osmotic stress, and oxidative stress were also abundant in the metagenome. Comparison of the composition of the functional community of the LH Spring to metagenomes from other saline/ subzero environments revealed a close association between the LH Spring and another Canadian high-Arctic permafrost environment, particularly in genes related to sulfur metabolism and dormancy. Overall, this study provides insights into the metabolic potential and the active microbial populations that exist in this hypersaline cryoenvironment and contributes to our understanding of microbial ecology in extreme environments. © 2013, American Society for Microbiology. Peer reviewed: Yes NRC publication: Yes
format Article in Journal/Newspaper
author Lay, C.-Y.
Mykytczuk, N.C.S.
Yergeau, É.
Lamarche-Gagnon, G.
Greer, C.W.
Whyte, L.G.
author_facet Lay, C.-Y.
Mykytczuk, N.C.S.
Yergeau, É.
Lamarche-Gagnon, G.
Greer, C.W.
Whyte, L.G.
author_sort Lay, C.-Y.
title Defining the functional potential and active community members of a sediment microbial community in a high-arctic hypersaline subzero spring
title_short Defining the functional potential and active community members of a sediment microbial community in a high-arctic hypersaline subzero spring
title_full Defining the functional potential and active community members of a sediment microbial community in a high-arctic hypersaline subzero spring
title_fullStr Defining the functional potential and active community members of a sediment microbial community in a high-arctic hypersaline subzero spring
title_full_unstemmed Defining the functional potential and active community members of a sediment microbial community in a high-arctic hypersaline subzero spring
title_sort defining the functional potential and active community members of a sediment microbial community in a high-arctic hypersaline subzero spring
publishDate 2013
url https://doi.org/10.1128/AEM.00153-13
https://nrc-publications.canada.ca/eng/view/object/?id=10066444-a0de-4d4f-8826-203bb06c265a
https://nrc-publications.canada.ca/fra/voir/objet/?id=10066444-a0de-4d4f-8826-203bb06c265a
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
permafrost
genre_facet Arctic
permafrost
op_relation issn:0099-2240
Applied and Environmental Microbiology, Volume: 79, Issue: 12, Publication date: 2013, Pages: 3637–3648
doi:10.1128/AEM.00153-13
op_doi https://doi.org/10.1128/AEM.00153-13
container_title Applied and Environmental Microbiology
container_volume 79
container_issue 12
container_start_page 3637
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