Organic carbon remobilized from thawing permafrost is resequestered by reactive iron on the Eurasian Arctic Shelf

Given the potential for permafrost carbon (PF/C)‐climate feedbacks in the Siberian‐Arctic land‐ocean system, there is a need for understanding the fate of thawed‐out PF/C. Here we show that the sequestration of OC by reactive iron (OC‐Fe) ranges between 0.5 and 22% on the Eurasian Arctic Shelf, with...

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Published in:Geophysical research letters Vol. 42; no. 19; pp. 8122 - 8130
Main Authors: Salvadó, Joan A., Tesi, Tommaso, Andersson, August, Ingri, Johan, Dudarev, Oleg V., Semiletov, Igor P., Gustafsson, Örjan
Format: Journal Article
Language:English
Published: Washington Blackwell Publishing Ltd 16-10-2015
John Wiley & Sons, Inc
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Summary:Given the potential for permafrost carbon (PF/C)‐climate feedbacks in the Siberian‐Arctic land‐ocean system, there is a need for understanding the fate of thawed‐out PF/C. Here we show that the sequestration of OC by reactive iron (OC‐Fe) ranges between 0.5 and 22% on the Eurasian Arctic Shelf, with higher values in the Kara Sea (KS) (18 ± 6%) and the Laptev Sea (LS) (14 ± 4%). The Δ14C/δ13C signatures of the OC‐Fe are substantially older and more terrestrial than the bulk sediment OC in the LS but younger and more dominated by marine plankton sources in the East Siberian Sea (ESS). Statistical source apportionment modeling reveal that reactive iron phases resequestered 15 ± 5% of thawing PF/C in the LS and 6.4 ± 5% in the ESS, derived from both coastal erosion of ice complex deposit and thawing topsoil. This Fe‐associated trap of PF/C constitutes a reduction of the degradation/outgassing and thus also an attenuation of the PF/C‐climate feedback. Key Points Insights on what OC fractions are trapped by reactive Fe phases The thawed PF/C is partly trapped by reactive Fe on the largest Arctic shelf This rusty carbon sink attenuates the PF/C‐climate feedback
Bibliography:EU financial support as a Marie Curie - No. FP7-PEOPLE-2012-IEF
ark:/67375/WNG-7CBSHKP4-M
Text S1, Tables S1 and S2, and Figures S1-S3
istex:3FC3A7246C97AE6C35F3CCB33E5CE04F9EED320B
ISMAR-CNR Sede di Bologna. I.P. Semiletov - No. #2013-220-04-157
Russian Scientific Foundation - No. 15-17-20032
US National Science Foundation - No. OPP ARC 0909546
ArticleID:GRL53546
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0094-8276
1944-8007
1944-8007
DOI:10.1002/2015GL066058