Biogeochemistry and timing of methane-derived carbonate formation at Leirdjupet fault complex, SW Barents sea
The origin of modern seafloor methane emissions in the Barents Sea is tightly connected to the glacio-tectonic and oceanographic transformations following the last ice age. Those regional events induced geological structure re-activation and destabilization of gas hydrate reservoirs over large areas...
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Online Access: | https://hdl.handle.net/10037/27146 https://doi.org/10.3389/feart.2022.1029471 |
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ftunivtroemsoe:oai:munin.uit.no:10037/27146 2023-05-15T15:38:27+02:00 Biogeochemistry and timing of methane-derived carbonate formation at Leirdjupet fault complex, SW Barents sea Argentino, Claudio Lee, Amicia Fallati, Luca Sahy, Diana Birgel, Daniel Peckmann, Jörn Bünz, Stefan Panieri, Giuliana 2022-10-25 https://hdl.handle.net/10037/27146 https://doi.org/10.3389/feart.2022.1029471 eng eng Frontiers Media Frontiers in Earth Science Argentino C, Lee AL, Fallati L, Sahy D, Birgel D, Peckmann J, Bünz S, Panieri G. Biogeochemistry and timing of methane-derived carbonate formation at Leirdjupet fault complex, SW Barents sea. Frontiers in Earth Science. 2022;10 FRIDAID 2064865 doi:10.3389/feart.2022.1029471 2296-6463 https://hdl.handle.net/10037/27146 Attribution 4.0 International (CC BY 4.0) openAccess Copyright 2022 The Author(s) https://creativecommons.org/licenses/by/4.0 CC-BY Journal article Tidsskriftartikkel Peer reviewed publishedVersion 2022 ftunivtroemsoe https://doi.org/10.3389/feart.2022.1029471 2022-11-03T00:01:18Z The origin of modern seafloor methane emissions in the Barents Sea is tightly connected to the glacio-tectonic and oceanographic transformations following the last ice age. Those regional events induced geological structure re-activation and destabilization of gas hydrate reservoirs over large areas of the European continental margins, sustaining widespread fluid plumbing systems. Despite the increasing number of new active seep discoveries, their accurate geochronology and paleo-dynamic is still poorly resolved, thus hindering precise identification of triggering factors and mechanisms controlling past and future seafloor emissions. Here, we report the distribution, petrographic (thin section, electron backscatter diffraction), isotopic (δ 13 C, δ 18 O) and lipid biomarker composition of methane-derived carbonates collected from Leirdjupet Fault Complex, SW Barents Sea, at 300 m depth during an ROV survey in 2021. Carbonates are located inside a 120 x 220 m elongated pockmark and form <10 m2 bodies protruding for about 2 m above the adjacent seafloor. Microstructural analyses of vein-filling cements showed the occurrence of three–five generations of isopachous aragonitic cement separated by dissolution surfaces indicative of intermittent oxidizing conditions. The integration of phase-specific isotopic analysis and U/Th dating showed δ 13 C values between −28.6‰ to −10.1‰ and δ 18 O between 4.6‰ and 5.3‰, enabling us to track carbonate mineral precipitation over the last ∼8 ka. Lipid biomarkers and their compound-specific δ 13 C analysis in the bulk carbonate revealed the presence of anaerobic methanotrophic archaea of the ANME-2 clade associated with sulfate-reducing bacteria of the Seep-SRB1 clade, as well as traces of petroleum. Our results indicate that methane and petroleum seepage in this area followed a similar evolution as in other southernmost Barents Sea sites controlled by the asynchronous deglaciation of the Barents Sea shelf, and that methane-derived carbonate precipitation is still an active ... Article in Journal/Newspaper Barents Sea University of Tromsø: Munin Open Research Archive Barents Sea Leirdjupet ENVELOPE(20.833,20.833,74.333,74.333) Frontiers in Earth Science 10 |
institution |
Open Polar |
collection |
University of Tromsø: Munin Open Research Archive |
op_collection_id |
ftunivtroemsoe |
language |
English |
description |
The origin of modern seafloor methane emissions in the Barents Sea is tightly connected to the glacio-tectonic and oceanographic transformations following the last ice age. Those regional events induced geological structure re-activation and destabilization of gas hydrate reservoirs over large areas of the European continental margins, sustaining widespread fluid plumbing systems. Despite the increasing number of new active seep discoveries, their accurate geochronology and paleo-dynamic is still poorly resolved, thus hindering precise identification of triggering factors and mechanisms controlling past and future seafloor emissions. Here, we report the distribution, petrographic (thin section, electron backscatter diffraction), isotopic (δ 13 C, δ 18 O) and lipid biomarker composition of methane-derived carbonates collected from Leirdjupet Fault Complex, SW Barents Sea, at 300 m depth during an ROV survey in 2021. Carbonates are located inside a 120 x 220 m elongated pockmark and form <10 m2 bodies protruding for about 2 m above the adjacent seafloor. Microstructural analyses of vein-filling cements showed the occurrence of three–five generations of isopachous aragonitic cement separated by dissolution surfaces indicative of intermittent oxidizing conditions. The integration of phase-specific isotopic analysis and U/Th dating showed δ 13 C values between −28.6‰ to −10.1‰ and δ 18 O between 4.6‰ and 5.3‰, enabling us to track carbonate mineral precipitation over the last ∼8 ka. Lipid biomarkers and their compound-specific δ 13 C analysis in the bulk carbonate revealed the presence of anaerobic methanotrophic archaea of the ANME-2 clade associated with sulfate-reducing bacteria of the Seep-SRB1 clade, as well as traces of petroleum. Our results indicate that methane and petroleum seepage in this area followed a similar evolution as in other southernmost Barents Sea sites controlled by the asynchronous deglaciation of the Barents Sea shelf, and that methane-derived carbonate precipitation is still an active ... |
format |
Article in Journal/Newspaper |
author |
Argentino, Claudio Lee, Amicia Fallati, Luca Sahy, Diana Birgel, Daniel Peckmann, Jörn Bünz, Stefan Panieri, Giuliana |
spellingShingle |
Argentino, Claudio Lee, Amicia Fallati, Luca Sahy, Diana Birgel, Daniel Peckmann, Jörn Bünz, Stefan Panieri, Giuliana Biogeochemistry and timing of methane-derived carbonate formation at Leirdjupet fault complex, SW Barents sea |
author_facet |
Argentino, Claudio Lee, Amicia Fallati, Luca Sahy, Diana Birgel, Daniel Peckmann, Jörn Bünz, Stefan Panieri, Giuliana |
author_sort |
Argentino, Claudio |
title |
Biogeochemistry and timing of methane-derived carbonate formation at Leirdjupet fault complex, SW Barents sea |
title_short |
Biogeochemistry and timing of methane-derived carbonate formation at Leirdjupet fault complex, SW Barents sea |
title_full |
Biogeochemistry and timing of methane-derived carbonate formation at Leirdjupet fault complex, SW Barents sea |
title_fullStr |
Biogeochemistry and timing of methane-derived carbonate formation at Leirdjupet fault complex, SW Barents sea |
title_full_unstemmed |
Biogeochemistry and timing of methane-derived carbonate formation at Leirdjupet fault complex, SW Barents sea |
title_sort |
biogeochemistry and timing of methane-derived carbonate formation at leirdjupet fault complex, sw barents sea |
publisher |
Frontiers Media |
publishDate |
2022 |
url |
https://hdl.handle.net/10037/27146 https://doi.org/10.3389/feart.2022.1029471 |
long_lat |
ENVELOPE(20.833,20.833,74.333,74.333) |
geographic |
Barents Sea Leirdjupet |
geographic_facet |
Barents Sea Leirdjupet |
genre |
Barents Sea |
genre_facet |
Barents Sea |
op_relation |
Frontiers in Earth Science Argentino C, Lee AL, Fallati L, Sahy D, Birgel D, Peckmann J, Bünz S, Panieri G. Biogeochemistry and timing of methane-derived carbonate formation at Leirdjupet fault complex, SW Barents sea. Frontiers in Earth Science. 2022;10 FRIDAID 2064865 doi:10.3389/feart.2022.1029471 2296-6463 https://hdl.handle.net/10037/27146 |
op_rights |
Attribution 4.0 International (CC BY 4.0) openAccess Copyright 2022 The Author(s) https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.3389/feart.2022.1029471 |
container_title |
Frontiers in Earth Science |
container_volume |
10 |
_version_ |
1766369387144544256 |