Electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost
Permafrost contains about 35% of the global soil organic carbon (0-3 m depth). As a consequence of global warming, the active layer thickness is steadily increasing and its organic carbon is becoming available for degradation, causing a concomitant release of CO2 and CH4. The climate forcing feedbac...
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ftuniaarhuspubl:oai:pure.atira.dk:publications/dd6629ed-df45-47bd-a4ec-a4868b5863e9 2023-05-15T13:03:11+02:00 Electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost Bak, Ebbe Norskov Jones, Eleanor Yde, Jacob Clement Hodson, Andy Mallon, Gunnar Finster, Kai 2017-04-26 https://pure.au.dk/portal/da/publications/electron-acceptorbased-regulation-of-microbial-greenhouse-gas-production-from-thawing-permafrost(dd6629ed-df45-47bd-a4ec-a4868b5863e9).html eng eng info:eu-repo/semantics/restrictedAccess Bak , E N , Jones , E , Yde , J C , Hodson , A , Mallon , G & Finster , K 2017 , ' Electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost ' , EGU 2017 , Wien , Austria , 24/04/2017 - 27/04/2017 . conferenceObject 2017 ftuniaarhuspubl 2022-12-21T23:54:41Z Permafrost contains about 35% of the global soil organic carbon (0-3 m depth). As a consequence of global warming, the active layer thickness is steadily increasing and its organic carbon is becoming available for degradation, causing a concomitant release of CO2 and CH4. The climate forcing feedbacks of permafrost thaw are determined by the rate of organic carbon degradation and to which degree it is released as CO2 or CH4. Methane is produced under anoxic conditions, but the factors that regulate its production are poorly constrained. In this study, we investigate how CH4 production is influenced by the presence of competing anaerobic processes with focus on the role of iron and sulfate reduction. We have collected permafrost cores to 2.2 meters depth from three different lowland sites in Adventdalen on Svalbard. From these cores, we have prepared anoxic batch incubation for each 25 cm depth interval and followed the production of CO2 and CH4 as well as the iron and sulfate reduction. This approach allows us to monitor the rate of the CO2 and CH4 production as well as to investigate the correlation between CH4 production and competing anaerobic respiration processes in the active layer as well in the permafrost. These investigations are accompanied by characterization of the carbon, iron and sulfate content in the soil and will be followed by characterization of the microbial community structure. The aim of this study is to get a better understanding of how the availability of sulfate and iron and the microbial community structure regulate the production of CO2 and CH4 in thawing permafrost, and to elucidate how the rate of the organic carbon degradation changes with depth in permafrost-affected soils. This study improves our understanding of climate feedback mechanisms operating during permafrost thaw. Conference Object Active layer thickness Adventdalen permafrost Svalbard Aarhus University: Research Adventdalen ENVELOPE(16.264,16.264,78.181,78.181) Svalbard |
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Open Polar |
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Aarhus University: Research |
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ftuniaarhuspubl |
language |
English |
description |
Permafrost contains about 35% of the global soil organic carbon (0-3 m depth). As a consequence of global warming, the active layer thickness is steadily increasing and its organic carbon is becoming available for degradation, causing a concomitant release of CO2 and CH4. The climate forcing feedbacks of permafrost thaw are determined by the rate of organic carbon degradation and to which degree it is released as CO2 or CH4. Methane is produced under anoxic conditions, but the factors that regulate its production are poorly constrained. In this study, we investigate how CH4 production is influenced by the presence of competing anaerobic processes with focus on the role of iron and sulfate reduction. We have collected permafrost cores to 2.2 meters depth from three different lowland sites in Adventdalen on Svalbard. From these cores, we have prepared anoxic batch incubation for each 25 cm depth interval and followed the production of CO2 and CH4 as well as the iron and sulfate reduction. This approach allows us to monitor the rate of the CO2 and CH4 production as well as to investigate the correlation between CH4 production and competing anaerobic respiration processes in the active layer as well in the permafrost. These investigations are accompanied by characterization of the carbon, iron and sulfate content in the soil and will be followed by characterization of the microbial community structure. The aim of this study is to get a better understanding of how the availability of sulfate and iron and the microbial community structure regulate the production of CO2 and CH4 in thawing permafrost, and to elucidate how the rate of the organic carbon degradation changes with depth in permafrost-affected soils. This study improves our understanding of climate feedback mechanisms operating during permafrost thaw. |
format |
Conference Object |
author |
Bak, Ebbe Norskov Jones, Eleanor Yde, Jacob Clement Hodson, Andy Mallon, Gunnar Finster, Kai |
spellingShingle |
Bak, Ebbe Norskov Jones, Eleanor Yde, Jacob Clement Hodson, Andy Mallon, Gunnar Finster, Kai Electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost |
author_facet |
Bak, Ebbe Norskov Jones, Eleanor Yde, Jacob Clement Hodson, Andy Mallon, Gunnar Finster, Kai |
author_sort |
Bak, Ebbe Norskov |
title |
Electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost |
title_short |
Electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost |
title_full |
Electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost |
title_fullStr |
Electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost |
title_full_unstemmed |
Electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost |
title_sort |
electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost |
publishDate |
2017 |
url |
https://pure.au.dk/portal/da/publications/electron-acceptorbased-regulation-of-microbial-greenhouse-gas-production-from-thawing-permafrost(dd6629ed-df45-47bd-a4ec-a4868b5863e9).html |
long_lat |
ENVELOPE(16.264,16.264,78.181,78.181) |
geographic |
Adventdalen Svalbard |
geographic_facet |
Adventdalen Svalbard |
genre |
Active layer thickness Adventdalen permafrost Svalbard |
genre_facet |
Active layer thickness Adventdalen permafrost Svalbard |
op_source |
Bak , E N , Jones , E , Yde , J C , Hodson , A , Mallon , G & Finster , K 2017 , ' Electron acceptor-based regulation of microbial greenhouse gas production from thawing permafrost ' , EGU 2017 , Wien , Austria , 24/04/2017 - 27/04/2017 . |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1766330717472555008 |