Nitrogen uptake by methanotrophic consortia in deep-water gas hydrate-bearing sediments

Methane-consuming microbes inhabiting marine methane seeps have recently been found to have the capacity to assimilate inorganic nitrogen, suggesting a previously unaccounted role in the global nitrogen cycle. Despite ex-situ experimental observations, definitive evidence of this process under in-si...

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Published in:Chemical Geology
Main Authors: Argentino, Claudio, Wittig, Cathrin, Peckmann, Jörn, Panieri, Giuliana
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2023
Subjects:
Online Access:https://hdl.handle.net/10037/29821
https://doi.org/10.1016/j.chemgeo.2023.121638
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/29821 2023-08-27T04:08:41+02:00 Nitrogen uptake by methanotrophic consortia in deep-water gas hydrate-bearing sediments Argentino, Claudio Wittig, Cathrin Peckmann, Jörn Panieri, Giuliana 2023-07-19 https://hdl.handle.net/10037/29821 https://doi.org/10.1016/j.chemgeo.2023.121638 eng eng Elsevier Chemical Geology Norges forskningsråd: 223259 Norges forskningsråd: 287869 Argentino C, Wittig C, Peckmann J, Panieri G. Nitrogen uptake by methanotrophic consortia in deep-water gas hydrate-bearing sediments. Chemical Geology. 2023;636 FRIDAID 2163397 doi:10.1016/j.chemgeo.2023.121638 0009-2541 1872-6836 https://hdl.handle.net/10037/29821 Attribution 4.0 International (CC BY 4.0) openAccess Copyright 2023 The Author(s) https://creativecommons.org/licenses/by/4.0 Journal article Tidsskriftartikkel Peer reviewed publishedVersion 2023 ftunivtroemsoe https://doi.org/10.1016/j.chemgeo.2023.121638 2023-08-09T23:07:01Z Methane-consuming microbes inhabiting marine methane seeps have recently been found to have the capacity to assimilate inorganic nitrogen, suggesting a previously unaccounted role in the global nitrogen cycle. Despite ex-situ experimental observations, definitive evidence of this process under in-situ conditions remains elusive, hindering the complete understanding of the controlling factors and magnitude of this process. We present the isotopic variations of organic carbon δ13Corg and total nitrogen δ15N values in two sediment cores collected from the gas hydrate-bearing Håkon Mosby Mud Volcano, SW Barents Sea (72°N, ∼1260 m water depth). We identified a stratigraphic interval containing methane-derived carbonates directly overlying a gas hydrate layer at 67 cm and typified by δ13Corg and δ15N as low as −42.0‰ and 1.2‰, respectively. Stable isotope mixing models confirm in-situ nitrogen uptake by methanotrophic consortia, contributing to up to 49.1 wt% of the local bulk sedimentary organic matter – a finding calling for reevaluation of the role of methane seeps in the oceanic nitrogen cycle Article in Journal/Newspaper Barents Sea University of Tromsø: Munin Open Research Archive Barents Sea Chemical Geology 636 121638
institution Open Polar
collection University of Tromsø: Munin Open Research Archive
op_collection_id ftunivtroemsoe
language English
description Methane-consuming microbes inhabiting marine methane seeps have recently been found to have the capacity to assimilate inorganic nitrogen, suggesting a previously unaccounted role in the global nitrogen cycle. Despite ex-situ experimental observations, definitive evidence of this process under in-situ conditions remains elusive, hindering the complete understanding of the controlling factors and magnitude of this process. We present the isotopic variations of organic carbon δ13Corg and total nitrogen δ15N values in two sediment cores collected from the gas hydrate-bearing Håkon Mosby Mud Volcano, SW Barents Sea (72°N, ∼1260 m water depth). We identified a stratigraphic interval containing methane-derived carbonates directly overlying a gas hydrate layer at 67 cm and typified by δ13Corg and δ15N as low as −42.0‰ and 1.2‰, respectively. Stable isotope mixing models confirm in-situ nitrogen uptake by methanotrophic consortia, contributing to up to 49.1 wt% of the local bulk sedimentary organic matter – a finding calling for reevaluation of the role of methane seeps in the oceanic nitrogen cycle
format Article in Journal/Newspaper
author Argentino, Claudio
Wittig, Cathrin
Peckmann, Jörn
Panieri, Giuliana
spellingShingle Argentino, Claudio
Wittig, Cathrin
Peckmann, Jörn
Panieri, Giuliana
Nitrogen uptake by methanotrophic consortia in deep-water gas hydrate-bearing sediments
author_facet Argentino, Claudio
Wittig, Cathrin
Peckmann, Jörn
Panieri, Giuliana
author_sort Argentino, Claudio
title Nitrogen uptake by methanotrophic consortia in deep-water gas hydrate-bearing sediments
title_short Nitrogen uptake by methanotrophic consortia in deep-water gas hydrate-bearing sediments
title_full Nitrogen uptake by methanotrophic consortia in deep-water gas hydrate-bearing sediments
title_fullStr Nitrogen uptake by methanotrophic consortia in deep-water gas hydrate-bearing sediments
title_full_unstemmed Nitrogen uptake by methanotrophic consortia in deep-water gas hydrate-bearing sediments
title_sort nitrogen uptake by methanotrophic consortia in deep-water gas hydrate-bearing sediments
publisher Elsevier
publishDate 2023
url https://hdl.handle.net/10037/29821
https://doi.org/10.1016/j.chemgeo.2023.121638
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
genre_facet Barents Sea
op_relation Chemical Geology
Norges forskningsråd: 223259
Norges forskningsråd: 287869
Argentino C, Wittig C, Peckmann J, Panieri G. Nitrogen uptake by methanotrophic consortia in deep-water gas hydrate-bearing sediments. Chemical Geology. 2023;636
FRIDAID 2163397
doi:10.1016/j.chemgeo.2023.121638
0009-2541
1872-6836
https://hdl.handle.net/10037/29821
op_rights Attribution 4.0 International (CC BY 4.0)
openAccess
Copyright 2023 The Author(s)
https://creativecommons.org/licenses/by/4.0
op_doi https://doi.org/10.1016/j.chemgeo.2023.121638
container_title Chemical Geology
container_volume 636
container_start_page 121638
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