Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming ...
During the last deglaciation (18–8 kyr BP), shelf flooding and warming presumably led to a large-scale decomposition of permafrost soils in the mid-to-high latitudes of the Northern Hemisphere. Microbial degradation of old organic matter released from the decomposing permafrost potentially contribut...
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Online Access: | https://dx.doi.org/10.3929/ethz-b-000358953 http://hdl.handle.net/20.500.11850/358953 |
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ftdatacite:10.3929/ethz-b-000358953 2024-04-28T08:14:37+00:00 Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming ... Meyer, Vera D. Hefter, Jens Köhler, Peter Tiedemann, Ralf Gersonde, Rainer Wacker, Lukas Mollenhauer, Gesine 2019 application/pdf https://dx.doi.org/10.3929/ethz-b-000358953 http://hdl.handle.net/20.500.11850/358953 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 deglaciation permafrost decomposition Beringia Bering Sea biomarker atmospheric CO2 Northwest Pacific article-journal Text ScholarlyArticle Journal Article 2019 ftdatacite https://doi.org/10.3929/ethz-b-000358953 2024-04-02T12:34:54Z During the last deglaciation (18–8 kyr BP), shelf flooding and warming presumably led to a large-scale decomposition of permafrost soils in the mid-to-high latitudes of the Northern Hemisphere. Microbial degradation of old organic matter released from the decomposing permafrost potentially contributed to the deglacial rise in atmospheric CO2 and also to the declining atmospheric radiocarbon contents (Δ14C). The significance of permafrost for the atmospheric carbon pool is not well understood as the timing of the carbon activation is poorly constrained by proxy data. Here, we trace the mobilization of organic matter from permafrost in the Pacific sector of Beringia over the last 22 kyr using mass-accumulation rates and radiocarbon signatures of terrigenous biomarkers in four sediment cores from the Bering Sea and the Northwest Pacific. We find that pronounced reworking and thus the vulnerability of old organic carbon to remineralization commenced during the early deglaciation (~16.8 kyr BP) when meltwater ... : Environmental Research Letters, 14 (8) ... Article in Journal/Newspaper Bering Sea permafrost Beringia DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
deglaciation permafrost decomposition Beringia Bering Sea biomarker atmospheric CO2 Northwest Pacific |
spellingShingle |
deglaciation permafrost decomposition Beringia Bering Sea biomarker atmospheric CO2 Northwest Pacific Meyer, Vera D. Hefter, Jens Köhler, Peter Tiedemann, Ralf Gersonde, Rainer Wacker, Lukas Mollenhauer, Gesine Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming ... |
topic_facet |
deglaciation permafrost decomposition Beringia Bering Sea biomarker atmospheric CO2 Northwest Pacific |
description |
During the last deglaciation (18–8 kyr BP), shelf flooding and warming presumably led to a large-scale decomposition of permafrost soils in the mid-to-high latitudes of the Northern Hemisphere. Microbial degradation of old organic matter released from the decomposing permafrost potentially contributed to the deglacial rise in atmospheric CO2 and also to the declining atmospheric radiocarbon contents (Δ14C). The significance of permafrost for the atmospheric carbon pool is not well understood as the timing of the carbon activation is poorly constrained by proxy data. Here, we trace the mobilization of organic matter from permafrost in the Pacific sector of Beringia over the last 22 kyr using mass-accumulation rates and radiocarbon signatures of terrigenous biomarkers in four sediment cores from the Bering Sea and the Northwest Pacific. We find that pronounced reworking and thus the vulnerability of old organic carbon to remineralization commenced during the early deglaciation (~16.8 kyr BP) when meltwater ... : Environmental Research Letters, 14 (8) ... |
format |
Article in Journal/Newspaper |
author |
Meyer, Vera D. Hefter, Jens Köhler, Peter Tiedemann, Ralf Gersonde, Rainer Wacker, Lukas Mollenhauer, Gesine |
author_facet |
Meyer, Vera D. Hefter, Jens Köhler, Peter Tiedemann, Ralf Gersonde, Rainer Wacker, Lukas Mollenhauer, Gesine |
author_sort |
Meyer, Vera D. |
title |
Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming ... |
title_short |
Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming ... |
title_full |
Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming ... |
title_fullStr |
Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming ... |
title_full_unstemmed |
Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming ... |
title_sort |
permafrost-carbon mobilization in beringia caused by deglacial meltwater runoff, sea-level rise and warming ... |
publisher |
ETH Zurich |
publishDate |
2019 |
url |
https://dx.doi.org/10.3929/ethz-b-000358953 http://hdl.handle.net/20.500.11850/358953 |
genre |
Bering Sea permafrost Beringia |
genre_facet |
Bering Sea permafrost Beringia |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.3929/ethz-b-000358953 |
_version_ |
1797580601440600064 |