Organic matter composition and greenhouse gas production of thawing subsea permafrost in the Laptev Sea
Subsea permafrost represents a large carbon pool that might be or become a significant greenhouse gas source. Scarcity of observational data causes large uncertainties. We here use five 21-56 m long subsea permafrost cores from the Laptev Sea to constrain organic carbon (OC) storage and sources, deg...
Published in: | Nature Communications |
---|---|
Main Authors: | , , , , , , , , , , , , , , |
Format: | Text |
Language: | English |
Published: |
Nature Publishing Group UK
2022
|
Subjects: | |
Online Access: | http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9420143/ http://www.ncbi.nlm.nih.gov/pubmed/36030269 https://doi.org/10.1038/s41467-022-32696-0 |
id |
ftpubmed:oai:pubmedcentral.nih.gov:9420143 |
---|---|
record_format |
openpolar |
spelling |
ftpubmed:oai:pubmedcentral.nih.gov:9420143 2023-05-15T17:07:13+02:00 Organic matter composition and greenhouse gas production of thawing subsea permafrost in the Laptev Sea Wild, Birgit Shakhova, Natalia Dudarev, Oleg Ruban, Alexey Kosmach, Denis Tumskoy, Vladimir Tesi, Tommaso Grimm, Hanna Nybom, Inna Matsubara, Felipe Alexanderson, Helena Jakobsson, Martin Mazurov, Alexey Semiletov, Igor Gustafsson, Örjan 2022-08-27 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9420143/ http://www.ncbi.nlm.nih.gov/pubmed/36030269 https://doi.org/10.1038/s41467-022-32696-0 en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9420143/ http://www.ncbi.nlm.nih.gov/pubmed/36030269 http://dx.doi.org/10.1038/s41467-022-32696-0 © The Author(s) 2022 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . CC-BY Nat Commun Article Text 2022 ftpubmed https://doi.org/10.1038/s41467-022-32696-0 2022-09-04T00:51:07Z Subsea permafrost represents a large carbon pool that might be or become a significant greenhouse gas source. Scarcity of observational data causes large uncertainties. We here use five 21-56 m long subsea permafrost cores from the Laptev Sea to constrain organic carbon (OC) storage and sources, degradation state and potential greenhouse gas production upon thaw. Grain sizes, optically-stimulated luminescence and biomarkers suggest deposition of aeolian silt and fluvial sand over 160 000 years, with dominant fluvial/alluvial deposition of forest- and tundra-derived organic matter. We estimate an annual thaw rate of 1.3 ± 0.6 kg OC m(−2) in subsea permafrost in the area, nine-fold exceeding organic carbon thaw rates for terrestrial permafrost. During 20-month incubations, CH(4) and CO(2) production averaged 1.7 nmol and 2.4 µmol g(−1) OC d(−1), providing a baseline to assess the contribution of subsea permafrost to the high CH(4) fluxes and strong ocean acidification observed in the region. Text laptev Laptev Sea Ocean acidification permafrost Tundra PubMed Central (PMC) Laptev Sea Nature Communications 13 1 |
institution |
Open Polar |
collection |
PubMed Central (PMC) |
op_collection_id |
ftpubmed |
language |
English |
topic |
Article |
spellingShingle |
Article Wild, Birgit Shakhova, Natalia Dudarev, Oleg Ruban, Alexey Kosmach, Denis Tumskoy, Vladimir Tesi, Tommaso Grimm, Hanna Nybom, Inna Matsubara, Felipe Alexanderson, Helena Jakobsson, Martin Mazurov, Alexey Semiletov, Igor Gustafsson, Örjan Organic matter composition and greenhouse gas production of thawing subsea permafrost in the Laptev Sea |
topic_facet |
Article |
description |
Subsea permafrost represents a large carbon pool that might be or become a significant greenhouse gas source. Scarcity of observational data causes large uncertainties. We here use five 21-56 m long subsea permafrost cores from the Laptev Sea to constrain organic carbon (OC) storage and sources, degradation state and potential greenhouse gas production upon thaw. Grain sizes, optically-stimulated luminescence and biomarkers suggest deposition of aeolian silt and fluvial sand over 160 000 years, with dominant fluvial/alluvial deposition of forest- and tundra-derived organic matter. We estimate an annual thaw rate of 1.3 ± 0.6 kg OC m(−2) in subsea permafrost in the area, nine-fold exceeding organic carbon thaw rates for terrestrial permafrost. During 20-month incubations, CH(4) and CO(2) production averaged 1.7 nmol and 2.4 µmol g(−1) OC d(−1), providing a baseline to assess the contribution of subsea permafrost to the high CH(4) fluxes and strong ocean acidification observed in the region. |
format |
Text |
author |
Wild, Birgit Shakhova, Natalia Dudarev, Oleg Ruban, Alexey Kosmach, Denis Tumskoy, Vladimir Tesi, Tommaso Grimm, Hanna Nybom, Inna Matsubara, Felipe Alexanderson, Helena Jakobsson, Martin Mazurov, Alexey Semiletov, Igor Gustafsson, Örjan |
author_facet |
Wild, Birgit Shakhova, Natalia Dudarev, Oleg Ruban, Alexey Kosmach, Denis Tumskoy, Vladimir Tesi, Tommaso Grimm, Hanna Nybom, Inna Matsubara, Felipe Alexanderson, Helena Jakobsson, Martin Mazurov, Alexey Semiletov, Igor Gustafsson, Örjan |
author_sort |
Wild, Birgit |
title |
Organic matter composition and greenhouse gas production of thawing subsea permafrost in the Laptev Sea |
title_short |
Organic matter composition and greenhouse gas production of thawing subsea permafrost in the Laptev Sea |
title_full |
Organic matter composition and greenhouse gas production of thawing subsea permafrost in the Laptev Sea |
title_fullStr |
Organic matter composition and greenhouse gas production of thawing subsea permafrost in the Laptev Sea |
title_full_unstemmed |
Organic matter composition and greenhouse gas production of thawing subsea permafrost in the Laptev Sea |
title_sort |
organic matter composition and greenhouse gas production of thawing subsea permafrost in the laptev sea |
publisher |
Nature Publishing Group UK |
publishDate |
2022 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9420143/ http://www.ncbi.nlm.nih.gov/pubmed/36030269 https://doi.org/10.1038/s41467-022-32696-0 |
geographic |
Laptev Sea |
geographic_facet |
Laptev Sea |
genre |
laptev Laptev Sea Ocean acidification permafrost Tundra |
genre_facet |
laptev Laptev Sea Ocean acidification permafrost Tundra |
op_source |
Nat Commun |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9420143/ http://www.ncbi.nlm.nih.gov/pubmed/36030269 http://dx.doi.org/10.1038/s41467-022-32696-0 |
op_rights |
© The Author(s) 2022 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/s41467-022-32696-0 |
container_title |
Nature Communications |
container_volume |
13 |
container_issue |
1 |
_version_ |
1766062517608513536 |