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...
Published in: | Environmental Research Letters |
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IOP Publishing
2019
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Online Access: | https://epic.awi.de/id/eprint/49980/ https://epic.awi.de/id/eprint/49980/1/meyer2019erl.pdf https://hdl.handle.net/10013/epic.ad252396-b701-48a2-b175-d44e34e9f85f https://hdl.handle.net/ |
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ftawi:oai:epic.awi.de:49980 2023-05-15T15:43:58+02:00 Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming Meyer, Vera D. Hefter, Jens H. Köhler, Peter Tiedemann, Ralf Gersonde, Rainer Wacker, Lukas Mollenhauer, Gesine 2019 application/pdf https://epic.awi.de/id/eprint/49980/ https://epic.awi.de/id/eprint/49980/1/meyer2019erl.pdf https://hdl.handle.net/10013/epic.ad252396-b701-48a2-b175-d44e34e9f85f https://hdl.handle.net/ unknown IOP Publishing https://epic.awi.de/id/eprint/49980/1/meyer2019erl.pdf https://hdl.handle.net/ Meyer, V. D. orcid:0000-0002-4958-5367 , Hefter, J. H. orcid:0000-0002-5823-1966 , Köhler, P. orcid:0000-0003-0904-8484 , Tiedemann, R. orcid:0000-0001-7211-8049 , Gersonde, R. , Wacker, L. and Mollenhauer, G. orcid:0000-0001-5138-564X (2019) Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming , Environmental Research Letters, 14 (8), 085003 . doi:10.1088/1748-9326/ab2653 <https://doi.org/10.1088/1748-9326%2Fab2653> , hdl:10013/epic.ad252396-b701-48a2-b175-d44e34e9f85f EPIC3Environmental Research Letters, IOP Publishing, 14(8), pp. 085003, ISSN: 1748-9326 Article isiRev 2019 ftawi https://doi.org/10.1088/1748-9326/ab2653 2021-12-24T15:44:50Z 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 runoff in the Yukon River intensified riverbank erosion of permafrost soils and fluvial discharge. Regional deglaciation in Alaska additionally mobilized significant fractions of fossil, petrogenic organic matter at this time. Permafrost decomposition across Beringia’s Pacific sector occurred in two major pulses that match the Bølling-Allerød and Preboreal warm spells and rapidly initiated within centuries. The carbon mobilization likely resulted from massive shelf flooding during meltwater pulses 1A (∼14.6 kyr BP) and 1B (∼11.5 kyr BP) followed by permafrost thaw in the hinterland. Our findings emphasize that coastal erosion was a major control to rapidly mobilize permafrost carbon along Beringia’s Pacific coast at ∼14.6 and ∼11.5 kyr BP implying that shelf flooding in Beringia may partly explain the centennial-scale rises in atmospheric CO2 at these times. Around 16.5 kyr BP, the mobilization of old terrigenous organic matter caused by meltwater-floods may have additionally contributed to increasing CO2 levels. Article in Journal/Newspaper Bering Sea permafrost Yukon river Alaska Beringia Yukon Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Bering Sea Pacific Yukon Environmental Research Letters 14 8 085003 |
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 |
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 runoff in the Yukon River intensified riverbank erosion of permafrost soils and fluvial discharge. Regional deglaciation in Alaska additionally mobilized significant fractions of fossil, petrogenic organic matter at this time. Permafrost decomposition across Beringia’s Pacific sector occurred in two major pulses that match the Bølling-Allerød and Preboreal warm spells and rapidly initiated within centuries. The carbon mobilization likely resulted from massive shelf flooding during meltwater pulses 1A (∼14.6 kyr BP) and 1B (∼11.5 kyr BP) followed by permafrost thaw in the hinterland. Our findings emphasize that coastal erosion was a major control to rapidly mobilize permafrost carbon along Beringia’s Pacific coast at ∼14.6 and ∼11.5 kyr BP implying that shelf flooding in Beringia may partly explain the centennial-scale rises in atmospheric CO2 at these times. Around 16.5 kyr BP, the mobilization of old terrigenous organic matter caused by meltwater-floods may have additionally contributed to increasing CO2 levels. |
format |
Article in Journal/Newspaper |
author |
Meyer, Vera D. Hefter, Jens H. Köhler, Peter Tiedemann, Ralf Gersonde, Rainer Wacker, Lukas Mollenhauer, Gesine |
spellingShingle |
Meyer, Vera D. Hefter, Jens H. 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 |
author_facet |
Meyer, Vera D. Hefter, Jens H. 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 |
IOP Publishing |
publishDate |
2019 |
url |
https://epic.awi.de/id/eprint/49980/ https://epic.awi.de/id/eprint/49980/1/meyer2019erl.pdf https://hdl.handle.net/10013/epic.ad252396-b701-48a2-b175-d44e34e9f85f https://hdl.handle.net/ |
geographic |
Bering Sea Pacific Yukon |
geographic_facet |
Bering Sea Pacific Yukon |
genre |
Bering Sea permafrost Yukon river Alaska Beringia Yukon |
genre_facet |
Bering Sea permafrost Yukon river Alaska Beringia Yukon |
op_source |
EPIC3Environmental Research Letters, IOP Publishing, 14(8), pp. 085003, ISSN: 1748-9326 |
op_relation |
https://epic.awi.de/id/eprint/49980/1/meyer2019erl.pdf https://hdl.handle.net/ Meyer, V. D. orcid:0000-0002-4958-5367 , Hefter, J. H. orcid:0000-0002-5823-1966 , Köhler, P. orcid:0000-0003-0904-8484 , Tiedemann, R. orcid:0000-0001-7211-8049 , Gersonde, R. , Wacker, L. and Mollenhauer, G. orcid:0000-0001-5138-564X (2019) Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming , Environmental Research Letters, 14 (8), 085003 . doi:10.1088/1748-9326/ab2653 <https://doi.org/10.1088/1748-9326%2Fab2653> , hdl:10013/epic.ad252396-b701-48a2-b175-d44e34e9f85f |
op_doi |
https://doi.org/10.1088/1748-9326/ab2653 |
container_title |
Environmental Research Letters |
container_volume |
14 |
container_issue |
8 |
container_start_page |
085003 |
_version_ |
1766378187757977600 |