Influence of Igneous Basement on Deep Sediment Microbial Diversity on the Eastern Juan de Fuca Ridge Flank
Microbial communities living in deeply buried sediment may be adapted to long-term energy limitation as they are removed from new detrital energy inputs for thousands to millions of years. However, sediment layers near the underlying oceanic crust may receive inputs from below that influence microbi...
Published in: | Frontiers in Microbiology |
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2017
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Online Access: | https://pure.au.dk/portal/da/publications/influence-of-igneous-basement-on-deep-sediment-microbial-diversity-on-the-eastern-juan-de-fuca-ridge-flank(60643ead-7a52-4acf-be78-a04a12da7765).html https://doi.org/10.3389/fmicb.2017.01434 |
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ftuniaarhuspubl:oai:pure.atira.dk:publications/60643ead-7a52-4acf-be78-a04a12da7765 2023-05-15T17:35:15+02:00 Influence of Igneous Basement on Deep Sediment Microbial Diversity on the Eastern Juan de Fuca Ridge Flank Labonte, Jessica M. Lever, Mark A. Edwards, Katrina J. Orcutt, Beth N. 2017-08-02 https://pure.au.dk/portal/da/publications/influence-of-igneous-basement-on-deep-sediment-microbial-diversity-on-the-eastern-juan-de-fuca-ridge-flank(60643ead-7a52-4acf-be78-a04a12da7765).html https://doi.org/10.3389/fmicb.2017.01434 eng eng info:eu-repo/semantics/restrictedAccess Labonte , J M , Lever , M A , Edwards , K J & Orcutt , B N 2017 , ' Influence of Igneous Basement on Deep Sediment Microbial Diversity on the Eastern Juan de Fuca Ridge Flank ' , Frontiers in Microbiology , vol. 8 , 1434 . https://doi.org/10.3389/fmicb.2017.01434 deep biosphere IODP basalt sediment Census of Deep Life MID-ATLANTIC RIDGE SEA-FLOOR SINGLE-CELL OCEAN CRUST SUBSEAFLOOR SEDIMENTS MARINE-SEDIMENTS BASALTIC CRUST NORTH-ATLANTIC WESTERN FLANK FLUIDS article 2017 ftuniaarhuspubl https://doi.org/10.3389/fmicb.2017.01434 2022-12-28T23:54:50Z Microbial communities living in deeply buried sediment may be adapted to long-term energy limitation as they are removed from new detrital energy inputs for thousands to millions of years. However, sediment layers near the underlying oceanic crust may receive inputs from below that influence microbial community structure and/or activity. As part of the Census of Deep Life, we used 16S rRNA gene tag pyrosequencing on DNA extracted from a spectrum of deep sediment-basement interface samples from the subsurface of the Juan de Fuca Ridge flank (collected on IODP Expedition 327) to examine this possible basement influence on deep sediment communities. This area experiences rapid sedimentation, with an underlying basaltic crust that hosts a dynamic flux of hydrothermal fluids that diffuse into the sediment. Chloroflexi sequences dominated tag libraries in all sediment samples, with variation in the abundance of other bacterial groups (e.g., Actinobacteria, Aerophobetes, Atribacteria, Planctomycetes, and Nitrospirae). These variations occur in relation to the type of sediment (clays versus carbonate-rich) and the depth of sample origin, and show no clear connection to the distance from the discharge outcrop or to basement fluid microbial communities. Actinobacteria-related sequences dominated the basalt libraries, but these should be viewed cautiously due to possibilities for imprinting from contamination. Our results indicate that proximity to basement or areas of seawater recharge is not a primary driver of microbial community composition in basal sediment, even though fluids diffusing from basement into sediment may stimulate microbial activity. Article in Journal/Newspaper North Atlantic Aarhus University: Research Mid-Atlantic Ridge Frontiers in Microbiology 8 |
institution |
Open Polar |
collection |
Aarhus University: Research |
op_collection_id |
ftuniaarhuspubl |
language |
English |
topic |
deep biosphere IODP basalt sediment Census of Deep Life MID-ATLANTIC RIDGE SEA-FLOOR SINGLE-CELL OCEAN CRUST SUBSEAFLOOR SEDIMENTS MARINE-SEDIMENTS BASALTIC CRUST NORTH-ATLANTIC WESTERN FLANK FLUIDS |
spellingShingle |
deep biosphere IODP basalt sediment Census of Deep Life MID-ATLANTIC RIDGE SEA-FLOOR SINGLE-CELL OCEAN CRUST SUBSEAFLOOR SEDIMENTS MARINE-SEDIMENTS BASALTIC CRUST NORTH-ATLANTIC WESTERN FLANK FLUIDS Labonte, Jessica M. Lever, Mark A. Edwards, Katrina J. Orcutt, Beth N. Influence of Igneous Basement on Deep Sediment Microbial Diversity on the Eastern Juan de Fuca Ridge Flank |
topic_facet |
deep biosphere IODP basalt sediment Census of Deep Life MID-ATLANTIC RIDGE SEA-FLOOR SINGLE-CELL OCEAN CRUST SUBSEAFLOOR SEDIMENTS MARINE-SEDIMENTS BASALTIC CRUST NORTH-ATLANTIC WESTERN FLANK FLUIDS |
description |
Microbial communities living in deeply buried sediment may be adapted to long-term energy limitation as they are removed from new detrital energy inputs for thousands to millions of years. However, sediment layers near the underlying oceanic crust may receive inputs from below that influence microbial community structure and/or activity. As part of the Census of Deep Life, we used 16S rRNA gene tag pyrosequencing on DNA extracted from a spectrum of deep sediment-basement interface samples from the subsurface of the Juan de Fuca Ridge flank (collected on IODP Expedition 327) to examine this possible basement influence on deep sediment communities. This area experiences rapid sedimentation, with an underlying basaltic crust that hosts a dynamic flux of hydrothermal fluids that diffuse into the sediment. Chloroflexi sequences dominated tag libraries in all sediment samples, with variation in the abundance of other bacterial groups (e.g., Actinobacteria, Aerophobetes, Atribacteria, Planctomycetes, and Nitrospirae). These variations occur in relation to the type of sediment (clays versus carbonate-rich) and the depth of sample origin, and show no clear connection to the distance from the discharge outcrop or to basement fluid microbial communities. Actinobacteria-related sequences dominated the basalt libraries, but these should be viewed cautiously due to possibilities for imprinting from contamination. Our results indicate that proximity to basement or areas of seawater recharge is not a primary driver of microbial community composition in basal sediment, even though fluids diffusing from basement into sediment may stimulate microbial activity. |
format |
Article in Journal/Newspaper |
author |
Labonte, Jessica M. Lever, Mark A. Edwards, Katrina J. Orcutt, Beth N. |
author_facet |
Labonte, Jessica M. Lever, Mark A. Edwards, Katrina J. Orcutt, Beth N. |
author_sort |
Labonte, Jessica M. |
title |
Influence of Igneous Basement on Deep Sediment Microbial Diversity on the Eastern Juan de Fuca Ridge Flank |
title_short |
Influence of Igneous Basement on Deep Sediment Microbial Diversity on the Eastern Juan de Fuca Ridge Flank |
title_full |
Influence of Igneous Basement on Deep Sediment Microbial Diversity on the Eastern Juan de Fuca Ridge Flank |
title_fullStr |
Influence of Igneous Basement on Deep Sediment Microbial Diversity on the Eastern Juan de Fuca Ridge Flank |
title_full_unstemmed |
Influence of Igneous Basement on Deep Sediment Microbial Diversity on the Eastern Juan de Fuca Ridge Flank |
title_sort |
influence of igneous basement on deep sediment microbial diversity on the eastern juan de fuca ridge flank |
publishDate |
2017 |
url |
https://pure.au.dk/portal/da/publications/influence-of-igneous-basement-on-deep-sediment-microbial-diversity-on-the-eastern-juan-de-fuca-ridge-flank(60643ead-7a52-4acf-be78-a04a12da7765).html https://doi.org/10.3389/fmicb.2017.01434 |
geographic |
Mid-Atlantic Ridge |
geographic_facet |
Mid-Atlantic Ridge |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Labonte , J M , Lever , M A , Edwards , K J & Orcutt , B N 2017 , ' Influence of Igneous Basement on Deep Sediment Microbial Diversity on the Eastern Juan de Fuca Ridge Flank ' , Frontiers in Microbiology , vol. 8 , 1434 . https://doi.org/10.3389/fmicb.2017.01434 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.3389/fmicb.2017.01434 |
container_title |
Frontiers in Microbiology |
container_volume |
8 |
_version_ |
1766134341222531072 |