New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments

Faust, Johan C.; Ascough, Philippa; Hilton, Robert G.; Stevenson, Mark; Hendry, Katherine R. ORCID: https://orcid.org/0000-0002-0790-5895; März, Christian. 2022 New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments. Environmental Research Letters, 18 (1), 014006. 12, pp. https://doi.org/10.1088/1748-9326/aca780

Before downloading, please read NORA policies.

Preview

Text (Open Access)
© 2022 The Author(s). Published by IOP Publishing Ltd.
Faust_2023_Environ._Res._Lett._18_014006.pdf - Published Version
Available under License Creative Commons Attribution 4.0.
Download (1MB) | Preview

Official URL: https://iopscience.iop.org/article/10.1088/1748-93...

Abstract/Summary

The protection of organic carbon through association with iron minerals (FeR) is an important factor in its stabilisation, long-term storage, and burial efficiency in marine sediments. However, large uncertainties still exist concerning the sources, lability, age, and composition of the organic matter associated with FeR in natural sediments. Therefore, the timing and environmental setting of the carbon-iron bonding process remain elusive. Here we use radiocarbon (Δ14C) and stable isotopes (δ13C) of downcore bulk sedimentary organic matter, benthic foraminifera and the organic carbon fraction bound to FeR to interrogate the source and age of the organic carbon pool associated with FeR in Arctic marine sediments. In the Barents Sea, we find that the organic carbon associated with FeR is younger overall than the bulk organic matter and is probably marine derived. The comparison to other investigations of OC-FeR origins reveals that in large parts of Arctic shelf regions FeR associated organic carbon is radiocarbon enriched and has a higher δ13Corg value compared to the bulk sediment, irrespective of sediment depth/age. Our findings suggest a rapid and preferential binding of fresh and marine organic matter with FeR. Hence, labile organic matter prone to decomposition is protected and stabilised, underlining the potential of the organic carbon-iron association as an efficient carbon burial mechanism.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1088/1748-9326/aca780
ISSN:	17489326
Additional Keywords:	Barents Sea, OC-Fe, Marine Shelf Sediments, Radiocarbon, Carbon Isotopes, Carbon Sequestration
Date made live:	01 Dec 2022 12:05 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/532712

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1088/1748-9326/aca780

ISSN:

17489326

Additional Keywords:

Barents Sea, OC-Fe, Marine Shelf Sediments, Radiocarbon, Carbon Isotopes, Carbon Sequestration

Date made live:

01 Dec 2022 12:05 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/532712