New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments
The protection of organic carbon through association with iron minerals (Fe _R ) 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 m...
Published in: | Environmental Research Letters |
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ftdoajarticles:oai:doaj.org/article:46f586e8c86246e3aa177ef163062227 2023-09-05T13:17:03+02:00 New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments Johan C Faust Philippa Ascough Robert G Hilton Mark A Stevenson Katharine R Hendry Christian März 2022-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/aca780 https://doaj.org/article/46f586e8c86246e3aa177ef163062227 EN eng IOP Publishing https://doi.org/10.1088/1748-9326/aca780 https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/aca780 1748-9326 https://doaj.org/article/46f586e8c86246e3aa177ef163062227 Environmental Research Letters, Vol 18, Iss 1, p 014006 (2022) Barents Sea OC-Fe marine shelf sediments radiocarbon carbon isotopes carbon sequestration Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2022 ftdoajarticles https://doi.org/10.1088/1748-9326/aca780 2023-08-13T00:36:51Z The protection of organic carbon through association with iron minerals (Fe _R ) 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 Fe _R in natural sediments. Therefore, the timing and environmental setting of the carbon-iron bonding process remain elusive. Here we use radiocarbon (Δ ^14 C) and stable isotopes (δ ^13 C) of downcore bulk sedimentary organic matter, benthic foraminifera and the organic carbon fraction bound to Fe _R to interrogate the source and age of the organic carbon pool associated with Fe _R in Arctic marine sediments. In the Barents Sea, we find that the organic carbon associated with Fe _R is younger overall than the bulk organic matter and is probably marine derived. The comparison to other investigations of OC-Fe _R origins reveals that in large parts of Arctic shelf regions Fe _R associated organic carbon is radiocarbon enriched and has a higher δ ^13 C _org 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 Fe _R . 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. Article in Journal/Newspaper Arctic Barents Sea Foraminifera* Directory of Open Access Journals: DOAJ Articles Arctic Barents Sea Environmental Research Letters 18 1 014006 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Barents Sea OC-Fe marine shelf sediments radiocarbon carbon isotopes carbon sequestration Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
spellingShingle |
Barents Sea OC-Fe marine shelf sediments radiocarbon carbon isotopes carbon sequestration Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 Johan C Faust Philippa Ascough Robert G Hilton Mark A Stevenson Katharine R Hendry Christian März New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments |
topic_facet |
Barents Sea OC-Fe marine shelf sediments radiocarbon carbon isotopes carbon sequestration Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
description |
The protection of organic carbon through association with iron minerals (Fe _R ) 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 Fe _R in natural sediments. Therefore, the timing and environmental setting of the carbon-iron bonding process remain elusive. Here we use radiocarbon (Δ ^14 C) and stable isotopes (δ ^13 C) of downcore bulk sedimentary organic matter, benthic foraminifera and the organic carbon fraction bound to Fe _R to interrogate the source and age of the organic carbon pool associated with Fe _R in Arctic marine sediments. In the Barents Sea, we find that the organic carbon associated with Fe _R is younger overall than the bulk organic matter and is probably marine derived. The comparison to other investigations of OC-Fe _R origins reveals that in large parts of Arctic shelf regions Fe _R associated organic carbon is radiocarbon enriched and has a higher δ ^13 C _org 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 Fe _R . 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. |
format |
Article in Journal/Newspaper |
author |
Johan C Faust Philippa Ascough Robert G Hilton Mark A Stevenson Katharine R Hendry Christian März |
author_facet |
Johan C Faust Philippa Ascough Robert G Hilton Mark A Stevenson Katharine R Hendry Christian März |
author_sort |
Johan C Faust |
title |
New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments |
title_short |
New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments |
title_full |
New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments |
title_fullStr |
New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments |
title_full_unstemmed |
New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments |
title_sort |
new evidence for preservation of contemporary marine organic carbon by iron in arctic shelf sediments |
publisher |
IOP Publishing |
publishDate |
2022 |
url |
https://doi.org/10.1088/1748-9326/aca780 https://doaj.org/article/46f586e8c86246e3aa177ef163062227 |
geographic |
Arctic Barents Sea |
geographic_facet |
Arctic Barents Sea |
genre |
Arctic Barents Sea Foraminifera* |
genre_facet |
Arctic Barents Sea Foraminifera* |
op_source |
Environmental Research Letters, Vol 18, Iss 1, p 014006 (2022) |
op_relation |
https://doi.org/10.1088/1748-9326/aca780 https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/aca780 1748-9326 https://doaj.org/article/46f586e8c86246e3aa177ef163062227 |
op_doi |
https://doi.org/10.1088/1748-9326/aca780 |
container_title |
Environmental Research Letters |
container_volume |
18 |
container_issue |
1 |
container_start_page |
014006 |
_version_ |
1776198387011420160 |