Carbon degradation and potential greenhouse gas production in a changing Arctic thermokarst landscape

Permafrost carbon pools are vulnerable to a warming climate and bear the potential to alter the terrestrial carbon cycle. In the extensive drained lake basins that span across Arctic lowlands, enhanced degradation of organic-rich deposits upon permafrost thaw could lead to greenhouse gas emissions t...

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Main Authors: Bischoff, Verena, Strauss, Jens, Lantuit, Hugues Benjamin, Liebner, Susanne, Wolter, Juliane
Format: Conference Object
Language:unknown
Published: 2023
Subjects:
Online Access:https://epic.awi.de/id/eprint/57862/
https://epic.awi.de/id/eprint/57862/1/Bischoff_EUCOP2023-ABSTRACTS-9.pdf
https://hdl.handle.net/10013/epic.718eec65-59e8-4041-a371-3a0a10f02ec6
id ftawi:oai:epic.awi.de:57862
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spelling ftawi:oai:epic.awi.de:57862 2024-02-27T08:36:17+00:00 Carbon degradation and potential greenhouse gas production in a changing Arctic thermokarst landscape Bischoff, Verena Strauss, Jens Lantuit, Hugues Benjamin Liebner, Susanne Wolter, Juliane 2023-06-22 application/pdf https://epic.awi.de/id/eprint/57862/ https://epic.awi.de/id/eprint/57862/1/Bischoff_EUCOP2023-ABSTRACTS-9.pdf https://hdl.handle.net/10013/epic.718eec65-59e8-4041-a371-3a0a10f02ec6 unknown https://epic.awi.de/id/eprint/57862/1/Bischoff_EUCOP2023-ABSTRACTS-9.pdf Bischoff, V. , Strauss, J. orcid:0000-0003-4678-4982 , Lantuit, H. B. orcid:0000-0003-1497-6760 , Liebner, S. and Wolter, J. (2023) Carbon degradation and potential greenhouse gas production in a changing Arctic thermokarst landscape hdl:10013/epic.718eec65-59e8-4041-a371-3a0a10f02ec6 EPIC3 Conference NonPeerReviewed 2023 ftawi 2024-01-29T00:23:10Z Permafrost carbon pools are vulnerable to a warming climate and bear the potential to alter the terrestrial carbon cycle. In the extensive drained lake basins that span across Arctic lowlands, enhanced degradation of organic-rich deposits upon permafrost thaw could lead to greenhouse gas emissions to the atmosphere. Yet, little is known on the geochemical properties of the sediments in these basins and on the rate of release of greenhouse gases. This study investigates processes and intensity of organic matter decomposition and associated potential greenhouse gas production in thawed sediment from drained lake basins on the Yukon Coastal Plain in the western Canadian Arctic. We conducted a three-month low temperature (4 °C) incubation experiment, during which we measured carbon dioxide (CO2) and methane (CH4) production in thawed sediment from two permafrost cores from adjacent drained lake basins. To simulate current and near future greenhouse gas production potential we incubated material from the active layer as well as from the transition layer and permafrost to account for projected active layer deepening. Four replicates of each sample were incubated under aerobic and anaerobic conditions, respectively. CO2 and CH4 concentrations were measured by gas chromatography. The experiment was supplemented by a comprehensive lipid biomarker analysis of the same sample material before and after the incubation covering n-alkanes, n-fatty acids, triterpenoids and hopanes. Biomarker concentrations and indices (average chain length, carbon preference index, higher-plant fatty acid index) gave insights on the origin and degradation state of organic matter as well as changes to carbon accompanying the incubation experiment. In a multi-proxy approach, findings are further aligned with biogeochemical and sedimentological parameters. Results will reveal organic matter vulnerability to decomposition and potential greenhouse gas production in sediments after thawing, both of which are key elements in assessing future ... Conference Object Arctic Arctic permafrost Thermokarst Yukon Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic Yukon
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Permafrost carbon pools are vulnerable to a warming climate and bear the potential to alter the terrestrial carbon cycle. In the extensive drained lake basins that span across Arctic lowlands, enhanced degradation of organic-rich deposits upon permafrost thaw could lead to greenhouse gas emissions to the atmosphere. Yet, little is known on the geochemical properties of the sediments in these basins and on the rate of release of greenhouse gases. This study investigates processes and intensity of organic matter decomposition and associated potential greenhouse gas production in thawed sediment from drained lake basins on the Yukon Coastal Plain in the western Canadian Arctic. We conducted a three-month low temperature (4 °C) incubation experiment, during which we measured carbon dioxide (CO2) and methane (CH4) production in thawed sediment from two permafrost cores from adjacent drained lake basins. To simulate current and near future greenhouse gas production potential we incubated material from the active layer as well as from the transition layer and permafrost to account for projected active layer deepening. Four replicates of each sample were incubated under aerobic and anaerobic conditions, respectively. CO2 and CH4 concentrations were measured by gas chromatography. The experiment was supplemented by a comprehensive lipid biomarker analysis of the same sample material before and after the incubation covering n-alkanes, n-fatty acids, triterpenoids and hopanes. Biomarker concentrations and indices (average chain length, carbon preference index, higher-plant fatty acid index) gave insights on the origin and degradation state of organic matter as well as changes to carbon accompanying the incubation experiment. In a multi-proxy approach, findings are further aligned with biogeochemical and sedimentological parameters. Results will reveal organic matter vulnerability to decomposition and potential greenhouse gas production in sediments after thawing, both of which are key elements in assessing future ...
format Conference Object
author Bischoff, Verena
Strauss, Jens
Lantuit, Hugues Benjamin
Liebner, Susanne
Wolter, Juliane
spellingShingle Bischoff, Verena
Strauss, Jens
Lantuit, Hugues Benjamin
Liebner, Susanne
Wolter, Juliane
Carbon degradation and potential greenhouse gas production in a changing Arctic thermokarst landscape
author_facet Bischoff, Verena
Strauss, Jens
Lantuit, Hugues Benjamin
Liebner, Susanne
Wolter, Juliane
author_sort Bischoff, Verena
title Carbon degradation and potential greenhouse gas production in a changing Arctic thermokarst landscape
title_short Carbon degradation and potential greenhouse gas production in a changing Arctic thermokarst landscape
title_full Carbon degradation and potential greenhouse gas production in a changing Arctic thermokarst landscape
title_fullStr Carbon degradation and potential greenhouse gas production in a changing Arctic thermokarst landscape
title_full_unstemmed Carbon degradation and potential greenhouse gas production in a changing Arctic thermokarst landscape
title_sort carbon degradation and potential greenhouse gas production in a changing arctic thermokarst landscape
publishDate 2023
url https://epic.awi.de/id/eprint/57862/
https://epic.awi.de/id/eprint/57862/1/Bischoff_EUCOP2023-ABSTRACTS-9.pdf
https://hdl.handle.net/10013/epic.718eec65-59e8-4041-a371-3a0a10f02ec6
geographic Arctic
Yukon
geographic_facet Arctic
Yukon
genre Arctic
Arctic
permafrost
Thermokarst
Yukon
genre_facet Arctic
Arctic
permafrost
Thermokarst
Yukon
op_source EPIC3
op_relation https://epic.awi.de/id/eprint/57862/1/Bischoff_EUCOP2023-ABSTRACTS-9.pdf
Bischoff, V. , Strauss, J. orcid:0000-0003-4678-4982 , Lantuit, H. B. orcid:0000-0003-1497-6760 , Liebner, S. and Wolter, J. (2023) Carbon degradation and potential greenhouse gas production in a changing Arctic thermokarst landscape hdl:10013/epic.718eec65-59e8-4041-a371-3a0a10f02ec6
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