Nitrogen Fixation Potential in Bathypelagic Sediment of the Ice-Covered Arctic Ocean Revealed Through Long-Term Stable Isotope Incubations.

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Main Authors: von Friesen, Lisa W, Löscher, Carolin R, Bertilsson, Stefan, Farnelid, Hanna, Snoeijs-Leijonmalm, Pauline, Sundbom, Marcus, Traving, Sachia J, Vermassen, Flor, Riemann, Lasse
Format: Artículo científico
Language:en
Published: Environmental microbiology reports 2025
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author von Friesen, Lisa W
Löscher, Carolin R
Bertilsson, Stefan
Farnelid, Hanna
Snoeijs-Leijonmalm, Pauline
Sundbom, Marcus
Traving, Sachia J
Vermassen, Flor
Riemann, Lasse
author_facet von Friesen, Lisa W
Löscher, Carolin R
Bertilsson, Stefan
Farnelid, Hanna
Snoeijs-Leijonmalm, Pauline
Sundbom, Marcus
Traving, Sachia J
Vermassen, Flor
Riemann, Lasse
von Friesen, Lisa W
Löscher, Carolin R
Bertilsson, Stefan
Farnelid, Hanna
Snoeijs-Leijonmalm, Pauline
Sundbom, Marcus
Traving, Sachia J
Vermassen, Flor
Riemann, Lasse
collection PubMed - marine biology
contents Nitrogen Fixation Potential in Bathypelagic Sediment of the Ice-Covered Arctic Ocean Revealed Through Long-Term Stable Isotope Incubations. von Friesen, Lisa W Löscher, Carolin R Bertilsson, Stefan Farnelid, Hanna Snoeijs-Leijonmalm, Pauline Sundbom, Marcus Traving, Sachia J Vermassen, Flor Riemann, Lasse Nitrogen Fixation Geologic Sediments Arctic Regions Ice Cover Nitrogen Isotopes Bacteria Seawater Oceans and Seas Phylogeny Oxidoreductases Nitrogen Due to climate change, sea ice more commonly retreats over the shelf breaks in the Arctic Ocean, impacting sea ice-pelagic-benthic coupling in the deeper basins. Nitrogen fixation (the reduction of dinitrogen gas to bioavailable ammonia by microorganisms called diazotrophs) is reported from Arctic shelf sediments but is unknown from the Arctic deep sea. We sampled five locations of deep-sea (900-1500 m) surface sediments in the central ice-covered Arctic Ocean to measure potential nitrogen fixation through long-term (> 280 days) stable-isotope (N) incubations and to study diazotroph community composition through amplicon sequencing of the functional marker gene nifH. We measured low but detectable nitrogen fixation rates at the Lomonosov Ridge (0.6 pmol N g day) and the Morris Jessup Rise (0.4 pmol N g day). Nitrogen fixation was observed in sediments with the lowest organic matter content and bacterial abundance, and where sulphate-reducers like Desulfuromonadia and Desulfosporosinus sp. were prominent. Most nifH genes were distantly related to known diazotrophs. In this study, we show a potential for nitrogen fixation in Arctic bathypelagic sediments, considerably extending the known biome of marine nitrogen fixation. It raises the question of the significance of low but potentially widespread nitrogen fixation in deep-sea sediments.
format Artículo científico
id pubmed_40906446
institution PubMed
language en
publishDate 2025
publisher Environmental microbiology reports
record_format pubmed
spellingShingle Nitrogen Fixation Potential in Bathypelagic Sediment of the Ice-Covered Arctic Ocean Revealed Through Long-Term Stable Isotope Incubations.
von Friesen, Lisa W
Löscher, Carolin R
Bertilsson, Stefan
Farnelid, Hanna
Snoeijs-Leijonmalm, Pauline
Sundbom, Marcus
Traving, Sachia J
Vermassen, Flor
Riemann, Lasse
Nitrogen Fixation
Geologic Sediments
Arctic Regions
Ice Cover
Nitrogen Isotopes
Bacteria
Seawater
Oceans and Seas
Phylogeny
Oxidoreductases
Nitrogen
Nitrogen Fixation Potential in Bathypelagic Sediment of the Ice-Covered Arctic Ocean Revealed Through Long-Term Stable Isotope Incubations. von Friesen, Lisa W Löscher, Carolin R Bertilsson, Stefan Farnelid, Hanna Snoeijs-Leijonmalm, Pauline Sundbom, Marcus Traving, Sachia J Vermassen, Flor Riemann, Lasse Nitrogen Fixation Geologic Sediments Arctic Regions Ice Cover Nitrogen Isotopes Bacteria Seawater Oceans and Seas Phylogeny Oxidoreductases Nitrogen Due to climate change, sea ice more commonly retreats over the shelf breaks in the Arctic Ocean, impacting sea ice-pelagic-benthic coupling in the deeper basins. Nitrogen fixation (the reduction of dinitrogen gas to bioavailable ammonia by microorganisms called diazotrophs) is reported from Arctic shelf sediments but is unknown from the Arctic deep sea. We sampled five locations of deep-sea (900-1500 m) surface sediments in the central ice-covered Arctic Ocean to measure potential nitrogen fixation through long-term (> 280 days) stable-isotope (N) incubations and to study diazotroph community composition through amplicon sequencing of the functional marker gene nifH. We measured low but detectable nitrogen fixation rates at the Lomonosov Ridge (0.6 pmol N g day) and the Morris Jessup Rise (0.4 pmol N g day). Nitrogen fixation was observed in sediments with the lowest organic matter content and bacterial abundance, and where sulphate-reducers like Desulfuromonadia and Desulfosporosinus sp. were prominent. Most nifH genes were distantly related to known diazotrophs. In this study, we show a potential for nitrogen fixation in Arctic bathypelagic sediments, considerably extending the known biome of marine nitrogen fixation. It raises the question of the significance of low but potentially widespread nitrogen fixation in deep-sea sediments.
title Nitrogen Fixation Potential in Bathypelagic Sediment of the Ice-Covered Arctic Ocean Revealed Through Long-Term Stable Isotope Incubations.
topic Nitrogen Fixation
Geologic Sediments
Arctic Regions
Ice Cover
Nitrogen Isotopes
Bacteria
Seawater
Oceans and Seas
Phylogeny
Oxidoreductases
Nitrogen
url https://pubmed.ncbi.nlm.nih.gov/40906446/