Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia
Permafrost deposits have been a sink for atmospheric carbon for millennia. Thaw-erosional processes, however, can lead to rapid degradation of ice-rich permafrost and the release of substantial amounts of organic carbon (OC). The amount of the OC stored in these deposits and their potential to be mi...
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Copernicus Publications
2018
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Online Access: | https://epic.awi.de/id/eprint/49206/ https://epic.awi.de/id/eprint/49206/1/Walz_2018_Biogeosciences.pdf https://doi.org/10.5194/bg-15-5423-2018 https://hdl.handle.net/10013/epic.0b539116-732c-438e-a985-5f862cbdf6a7 |
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ftawi:oai:epic.awi.de:49206 2024-09-09T19:44:24+00:00 Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia Walz, Josefine Knoblauch, Christian Tigges, Ronja Opel, Thomas Schirrmeister, Lutz Pfeiffer, Eva-Maria 2018-09-13 application/pdf https://epic.awi.de/id/eprint/49206/ https://epic.awi.de/id/eprint/49206/1/Walz_2018_Biogeosciences.pdf https://doi.org/10.5194/bg-15-5423-2018 https://hdl.handle.net/10013/epic.0b539116-732c-438e-a985-5f862cbdf6a7 unknown Copernicus Publications https://epic.awi.de/id/eprint/49206/1/Walz_2018_Biogeosciences.pdf Walz, J. , Knoblauch, C. , Tigges, R. , Opel, T. , Schirrmeister, L. orcid:0000-0001-9455-0596 and Pfeiffer, E. M. (2018) Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia , Biogeosciences, 15 (17), pp. 5423-5436 . doi:10.5194/bg-15-5423-2018 <https://doi.org/10.5194/bg-15-5423-2018> , hdl:10013/epic.0b539116-732c-438e-a985-5f862cbdf6a7 EPIC3Biogeosciences, Copernicus Publications, 15(17), pp. 5423-5436, ISSN: 1726-4189 Article isiRev 2018 ftawi https://doi.org/10.5194/bg-15-5423-2018 2024-06-24T04:22:11Z Permafrost deposits have been a sink for atmospheric carbon for millennia. Thaw-erosional processes, however, can lead to rapid degradation of ice-rich permafrost and the release of substantial amounts of organic carbon (OC). The amount of the OC stored in these deposits and their potential to be microbially decomposed to the greenhouse gases carbon dioxide (CO2) and methane (CH4) depends on climatic and environmental conditions during deposition and the decomposition history before incorporation into the permafrost. Here, we examine potential greenhouse gas production as a result of degrading ice-rich permafrost deposits from three locations in the northeastern Siberian Laptev Sea region. The deposits span a period of about 55 kyr from the last glacial period and Holocene interglacial. Samples from all three locations were incubated under aerobic and anaerobic conditions for 134 days at 4 °C. Greenhouse gas production was generally higher in deposits from glacial periods, where 0.2 %–6.1% of the initially available OC was decomposed to CO2. In contrast, only 0.1 %–4.0% of initial OC was decomposed in permafrost deposits from the Holocene and the late glacial transition. Within the deposits from the Kargin interstadial period (Marine Isotope Stage 3), local depositional environments, especially soil moisture, also affected the preservation of OC. Sediments deposited under wet conditions contained more labile OC and thus produced more greenhouse gases than sediments deposited under drier conditions. To assess the greenhouse gas production potentials over longer periods, deposits from two locations were incubated for a total of 785 days. However, more than 50% of total CO2 production over 785 days occurred within the first 134 days under aerobic conditions, while 80% were produced over the same period under anaerobic conditions, which emphasizes the nonlinearity of the OC decomposition processes. Methanogenesis was generally observed in active layer samples but only sporadically in permafrost samples and was ... Article in Journal/Newspaper Ice laptev Laptev Sea permafrost Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Laptev Sea Biogeosciences 15 17 5423 5436 |
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 deposits have been a sink for atmospheric carbon for millennia. Thaw-erosional processes, however, can lead to rapid degradation of ice-rich permafrost and the release of substantial amounts of organic carbon (OC). The amount of the OC stored in these deposits and their potential to be microbially decomposed to the greenhouse gases carbon dioxide (CO2) and methane (CH4) depends on climatic and environmental conditions during deposition and the decomposition history before incorporation into the permafrost. Here, we examine potential greenhouse gas production as a result of degrading ice-rich permafrost deposits from three locations in the northeastern Siberian Laptev Sea region. The deposits span a period of about 55 kyr from the last glacial period and Holocene interglacial. Samples from all three locations were incubated under aerobic and anaerobic conditions for 134 days at 4 °C. Greenhouse gas production was generally higher in deposits from glacial periods, where 0.2 %–6.1% of the initially available OC was decomposed to CO2. In contrast, only 0.1 %–4.0% of initial OC was decomposed in permafrost deposits from the Holocene and the late glacial transition. Within the deposits from the Kargin interstadial period (Marine Isotope Stage 3), local depositional environments, especially soil moisture, also affected the preservation of OC. Sediments deposited under wet conditions contained more labile OC and thus produced more greenhouse gases than sediments deposited under drier conditions. To assess the greenhouse gas production potentials over longer periods, deposits from two locations were incubated for a total of 785 days. However, more than 50% of total CO2 production over 785 days occurred within the first 134 days under aerobic conditions, while 80% were produced over the same period under anaerobic conditions, which emphasizes the nonlinearity of the OC decomposition processes. Methanogenesis was generally observed in active layer samples but only sporadically in permafrost samples and was ... |
format |
Article in Journal/Newspaper |
author |
Walz, Josefine Knoblauch, Christian Tigges, Ronja Opel, Thomas Schirrmeister, Lutz Pfeiffer, Eva-Maria |
spellingShingle |
Walz, Josefine Knoblauch, Christian Tigges, Ronja Opel, Thomas Schirrmeister, Lutz Pfeiffer, Eva-Maria Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia |
author_facet |
Walz, Josefine Knoblauch, Christian Tigges, Ronja Opel, Thomas Schirrmeister, Lutz Pfeiffer, Eva-Maria |
author_sort |
Walz, Josefine |
title |
Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia |
title_short |
Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia |
title_full |
Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia |
title_fullStr |
Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia |
title_full_unstemmed |
Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia |
title_sort |
greenhouse gas production in degrading ice-rich permafrost deposits in northeastern siberia |
publisher |
Copernicus Publications |
publishDate |
2018 |
url |
https://epic.awi.de/id/eprint/49206/ https://epic.awi.de/id/eprint/49206/1/Walz_2018_Biogeosciences.pdf https://doi.org/10.5194/bg-15-5423-2018 https://hdl.handle.net/10013/epic.0b539116-732c-438e-a985-5f862cbdf6a7 |
geographic |
Laptev Sea |
geographic_facet |
Laptev Sea |
genre |
Ice laptev Laptev Sea permafrost Siberia |
genre_facet |
Ice laptev Laptev Sea permafrost Siberia |
op_source |
EPIC3Biogeosciences, Copernicus Publications, 15(17), pp. 5423-5436, ISSN: 1726-4189 |
op_relation |
https://epic.awi.de/id/eprint/49206/1/Walz_2018_Biogeosciences.pdf Walz, J. , Knoblauch, C. , Tigges, R. , Opel, T. , Schirrmeister, L. orcid:0000-0001-9455-0596 and Pfeiffer, E. M. (2018) Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia , Biogeosciences, 15 (17), pp. 5423-5436 . doi:10.5194/bg-15-5423-2018 <https://doi.org/10.5194/bg-15-5423-2018> , hdl:10013/epic.0b539116-732c-438e-a985-5f862cbdf6a7 |
op_doi |
https://doi.org/10.5194/bg-15-5423-2018 |
container_title |
Biogeosciences |
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15 |
container_issue |
17 |
container_start_page |
5423 |
op_container_end_page |
5436 |
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1809914110866882560 |