Utilization, release, and long-term fate of ancient carbon from eroding permafrost coastlines
About 34% of global coast lines are underlain by permafrost. Rising temperatures cause an acceleration in erosion rates of up to 10s of meters annually, exporting increasing amounts of carbon and nutrients to the coastal ocean. The degradation of ancient organic carbon (OC) from permafrost is an imp...
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ftawi:oai:epic.awi.de:57859 2024-02-27T08:38:21+00:00 Utilization, release, and long-term fate of ancient carbon from eroding permafrost coastlines Ruben, Manuel Marchant, Hannah Wietz, Matthias Gentz, Torben Galy, Valier Bröder, Lisa Strauss, Jens Mollenhauer, Gesine 2023-06-22 application/pdf https://epic.awi.de/id/eprint/57859/ https://epic.awi.de/id/eprint/57859/1/Ruben_%20EUCOP2023-ABSTRACTS-4.pdf https://hdl.handle.net/10013/epic.270b6597-dead-4b2d-9eaf-682af09d7236 unknown https://epic.awi.de/id/eprint/57859/1/Ruben_%20EUCOP2023-ABSTRACTS-4.pdf Ruben, M. orcid:0000-0003-2618-6483 , Marchant, H. , Wietz, M. orcid:0000-0002-9786-3026 , Gentz, T. , Galy, V. , Bröder, L. , Strauss, J. orcid:0000-0003-4678-4982 and Mollenhauer, G. orcid:0000-0001-5138-564X (2023) Utilization, release, and long-term fate of ancient carbon from eroding permafrost coastlines hdl:10013/epic.270b6597-dead-4b2d-9eaf-682af09d7236 EPIC3 Conference NonPeerReviewed 2023 ftawi 2024-01-29T00:23:10Z About 34% of global coast lines are underlain by permafrost. Rising temperatures cause an acceleration in erosion rates of up to 10s of meters annually, exporting increasing amounts of carbon and nutrients to the coastal ocean. The degradation of ancient organic carbon (OC) from permafrost is an important potential feedback mechanism in a warming climate. However, little is known about permafrost OC degradation after entering the ocean and its long term-fate after redeposition on the sea floor. Some recent studies have revealed CO2 release to occur when ancient permafrost materials are incubated with sea water. However, despite its importance for carbon feedback mechanisms, no study has directly assessed whether this CO2 release is indeed derived from respiration of ancient permafrost OC. We used a multi-disciplinary approach incubating Yedoma permafrost from the Lena Delta in natural coastal seawater from the south-eastern Kara Sea. By combining biogeochemical analyses, DNA-sequencing, ramped oxidation, pyrolysis and stable and radiocarbon isotope analysis we were able to: 1) quantify CO2 emissions from permafrost utilization; 2) for the first time demonstrate the amount of ancient OC contributing to CO2 emissions; 3) link the processes to specific microbial communities; and 4) characterize and assess lability of permafrost OC after redeposition on the sea floor. Our data clearly indicate high bioavailability of permafrost OC and rapid utilization after thawed material has entered the water column, while observing only minor changes in permafrost OC composition over time. Microbial communities are distinctly different in suspended Yedoma particles and water. Overall, our results suggest that under anthropogenic Arctic warming, enhanced coastal erosion will result in increased greenhouse gas emissions, as formerly freeze-locked ancient permafrost OC is remineralized by microbial communities when released to the coastal ocean. Conference Object Arctic Kara Sea lena delta permafrost Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic Kara Sea |
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Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
About 34% of global coast lines are underlain by permafrost. Rising temperatures cause an acceleration in erosion rates of up to 10s of meters annually, exporting increasing amounts of carbon and nutrients to the coastal ocean. The degradation of ancient organic carbon (OC) from permafrost is an important potential feedback mechanism in a warming climate. However, little is known about permafrost OC degradation after entering the ocean and its long term-fate after redeposition on the sea floor. Some recent studies have revealed CO2 release to occur when ancient permafrost materials are incubated with sea water. However, despite its importance for carbon feedback mechanisms, no study has directly assessed whether this CO2 release is indeed derived from respiration of ancient permafrost OC. We used a multi-disciplinary approach incubating Yedoma permafrost from the Lena Delta in natural coastal seawater from the south-eastern Kara Sea. By combining biogeochemical analyses, DNA-sequencing, ramped oxidation, pyrolysis and stable and radiocarbon isotope analysis we were able to: 1) quantify CO2 emissions from permafrost utilization; 2) for the first time demonstrate the amount of ancient OC contributing to CO2 emissions; 3) link the processes to specific microbial communities; and 4) characterize and assess lability of permafrost OC after redeposition on the sea floor. Our data clearly indicate high bioavailability of permafrost OC and rapid utilization after thawed material has entered the water column, while observing only minor changes in permafrost OC composition over time. Microbial communities are distinctly different in suspended Yedoma particles and water. Overall, our results suggest that under anthropogenic Arctic warming, enhanced coastal erosion will result in increased greenhouse gas emissions, as formerly freeze-locked ancient permafrost OC is remineralized by microbial communities when released to the coastal ocean. |
format |
Conference Object |
author |
Ruben, Manuel Marchant, Hannah Wietz, Matthias Gentz, Torben Galy, Valier Bröder, Lisa Strauss, Jens Mollenhauer, Gesine |
spellingShingle |
Ruben, Manuel Marchant, Hannah Wietz, Matthias Gentz, Torben Galy, Valier Bröder, Lisa Strauss, Jens Mollenhauer, Gesine Utilization, release, and long-term fate of ancient carbon from eroding permafrost coastlines |
author_facet |
Ruben, Manuel Marchant, Hannah Wietz, Matthias Gentz, Torben Galy, Valier Bröder, Lisa Strauss, Jens Mollenhauer, Gesine |
author_sort |
Ruben, Manuel |
title |
Utilization, release, and long-term fate of ancient carbon from eroding permafrost coastlines |
title_short |
Utilization, release, and long-term fate of ancient carbon from eroding permafrost coastlines |
title_full |
Utilization, release, and long-term fate of ancient carbon from eroding permafrost coastlines |
title_fullStr |
Utilization, release, and long-term fate of ancient carbon from eroding permafrost coastlines |
title_full_unstemmed |
Utilization, release, and long-term fate of ancient carbon from eroding permafrost coastlines |
title_sort |
utilization, release, and long-term fate of ancient carbon from eroding permafrost coastlines |
publishDate |
2023 |
url |
https://epic.awi.de/id/eprint/57859/ https://epic.awi.de/id/eprint/57859/1/Ruben_%20EUCOP2023-ABSTRACTS-4.pdf https://hdl.handle.net/10013/epic.270b6597-dead-4b2d-9eaf-682af09d7236 |
geographic |
Arctic Kara Sea |
geographic_facet |
Arctic Kara Sea |
genre |
Arctic Kara Sea lena delta permafrost |
genre_facet |
Arctic Kara Sea lena delta permafrost |
op_source |
EPIC3 |
op_relation |
https://epic.awi.de/id/eprint/57859/1/Ruben_%20EUCOP2023-ABSTRACTS-4.pdf Ruben, M. orcid:0000-0003-2618-6483 , Marchant, H. , Wietz, M. orcid:0000-0002-9786-3026 , Gentz, T. , Galy, V. , Bröder, L. , Strauss, J. orcid:0000-0003-4678-4982 and Mollenhauer, G. orcid:0000-0001-5138-564X (2023) Utilization, release, and long-term fate of ancient carbon from eroding permafrost coastlines hdl:10013/epic.270b6597-dead-4b2d-9eaf-682af09d7236 |
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1792045250366144512 |