Sources of dissolved iron to oxygen minimum zone waters on the Senegalese continental margin in the tropical North Atlantic Ocean: Insights from iron isotopes
Oxygen minimum zones (OMZs) cover extensive areas of eastern boundary ocean regions and play an important role in the cycling of the essential micronutrient iron (Fe). The isotopic composition of dissolved Fe (dFe) in shelf and slope waters on the Senegalese margin was determined to investigate the...
Published in: | Geochimica et Cosmochimica Acta |
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ftplymouthml:oai:plymsea.ac.uk:7923 2023-05-15T17:29:01+02:00 Sources of dissolved iron to oxygen minimum zone waters on the Senegalese continental margin in the tropical North Atlantic Ocean: Insights from iron isotopes Klar, JK Schlosser, C Milton, JA Woodward, EMS Lacan, F Parkinson, H Achterberg, EP James, RH 2018-03-02 text http://plymsea.ac.uk/id/eprint/7923/ http://plymsea.ac.uk/id/eprint/7923/7/GCA-S-17-00837%282%29.pdf https://www.sciencedirect.com/science/article/pii/S0016703718301133?via%3Dihub https://doi.org/10.1016/j.gca.2018.02.031 en eng http://plymsea.ac.uk/id/eprint/7923/7/GCA-S-17-00837%282%29.pdf Klar, JK; Schlosser, C; Milton, JA; Woodward, EMS; Lacan, F; Parkinson, H; Achterberg, EP; James, RH. 2018 Sources of dissolved iron to oxygen minimum zone waters on the Senegalese continental margin in the tropical North Atlantic Ocean: Insights from iron isotopes. Geochimica Et Cosmochimica Acta. https://doi.org/10.1016/j.gca.2018.02.031 <https://doi.org/10.1016/j.gca.2018.02.031> cc_by_nc_nd_4 CC-BY-NC-ND Chemistry Marine Sciences Oceanography Publication - Article PeerReviewed 2018 ftplymouthml https://doi.org/10.1016/j.gca.2018.02.031 2022-09-13T05:49:11Z Oxygen minimum zones (OMZs) cover extensive areas of eastern boundary ocean regions and play an important role in the cycling of the essential micronutrient iron (Fe). The isotopic composition of dissolved Fe (dFe) in shelf and slope waters on the Senegalese margin was determined to investigate the processes leading to enhanced dFe concentrations (up to 2 nM) in this tropical North Atlantic OMZ. On the shelf, the δ56Fe value of dFe (relative to the reference material IRMM-014) was as low as −0.33‰, which can be attributed to input of dFe from both reductive and nonreductive dissolution of sediments. Benthic inputs of dFe are subsequently upwelled to surface waters and recycled in the water column by biological uptake and remineralisation processes. Remineralised dFe is characterised by relatively high δ56Fe values (up to +0.41‰), and the contribution of remineralised Fe to the total dFe pool increases with distance from the shelf. Remineralisation plays an important role in the redistribution of dFe that is mainly supplied by benthic and atmospheric inputs, although dust inputs, estimated from dissolved aluminium concentrations, were low at the time of our study (2–9 nmol dFe m−2 d−1). As OMZs are expected to expand as climate warms, our data provide important insights into Fe sources and Fe cycling in the tropical North Atlantic Ocean. Article in Journal/Newspaper North Atlantic Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML) Geochimica et Cosmochimica Acta 236 60 78 |
institution |
Open Polar |
collection |
Plymouth Marine Science Electronic Archive (PlyMSEA - Plymouth Marine Laboratory, PML) |
op_collection_id |
ftplymouthml |
language |
English |
topic |
Chemistry Marine Sciences Oceanography |
spellingShingle |
Chemistry Marine Sciences Oceanography Klar, JK Schlosser, C Milton, JA Woodward, EMS Lacan, F Parkinson, H Achterberg, EP James, RH Sources of dissolved iron to oxygen minimum zone waters on the Senegalese continental margin in the tropical North Atlantic Ocean: Insights from iron isotopes |
topic_facet |
Chemistry Marine Sciences Oceanography |
description |
Oxygen minimum zones (OMZs) cover extensive areas of eastern boundary ocean regions and play an important role in the cycling of the essential micronutrient iron (Fe). The isotopic composition of dissolved Fe (dFe) in shelf and slope waters on the Senegalese margin was determined to investigate the processes leading to enhanced dFe concentrations (up to 2 nM) in this tropical North Atlantic OMZ. On the shelf, the δ56Fe value of dFe (relative to the reference material IRMM-014) was as low as −0.33‰, which can be attributed to input of dFe from both reductive and nonreductive dissolution of sediments. Benthic inputs of dFe are subsequently upwelled to surface waters and recycled in the water column by biological uptake and remineralisation processes. Remineralised dFe is characterised by relatively high δ56Fe values (up to +0.41‰), and the contribution of remineralised Fe to the total dFe pool increases with distance from the shelf. Remineralisation plays an important role in the redistribution of dFe that is mainly supplied by benthic and atmospheric inputs, although dust inputs, estimated from dissolved aluminium concentrations, were low at the time of our study (2–9 nmol dFe m−2 d−1). As OMZs are expected to expand as climate warms, our data provide important insights into Fe sources and Fe cycling in the tropical North Atlantic Ocean. |
format |
Article in Journal/Newspaper |
author |
Klar, JK Schlosser, C Milton, JA Woodward, EMS Lacan, F Parkinson, H Achterberg, EP James, RH |
author_facet |
Klar, JK Schlosser, C Milton, JA Woodward, EMS Lacan, F Parkinson, H Achterberg, EP James, RH |
author_sort |
Klar, JK |
title |
Sources of dissolved iron to oxygen minimum zone waters on the Senegalese continental margin in the tropical North Atlantic Ocean: Insights from iron isotopes |
title_short |
Sources of dissolved iron to oxygen minimum zone waters on the Senegalese continental margin in the tropical North Atlantic Ocean: Insights from iron isotopes |
title_full |
Sources of dissolved iron to oxygen minimum zone waters on the Senegalese continental margin in the tropical North Atlantic Ocean: Insights from iron isotopes |
title_fullStr |
Sources of dissolved iron to oxygen minimum zone waters on the Senegalese continental margin in the tropical North Atlantic Ocean: Insights from iron isotopes |
title_full_unstemmed |
Sources of dissolved iron to oxygen minimum zone waters on the Senegalese continental margin in the tropical North Atlantic Ocean: Insights from iron isotopes |
title_sort |
sources of dissolved iron to oxygen minimum zone waters on the senegalese continental margin in the tropical north atlantic ocean: insights from iron isotopes |
publishDate |
2018 |
url |
http://plymsea.ac.uk/id/eprint/7923/ http://plymsea.ac.uk/id/eprint/7923/7/GCA-S-17-00837%282%29.pdf https://www.sciencedirect.com/science/article/pii/S0016703718301133?via%3Dihub https://doi.org/10.1016/j.gca.2018.02.031 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
http://plymsea.ac.uk/id/eprint/7923/7/GCA-S-17-00837%282%29.pdf Klar, JK; Schlosser, C; Milton, JA; Woodward, EMS; Lacan, F; Parkinson, H; Achterberg, EP; James, RH. 2018 Sources of dissolved iron to oxygen minimum zone waters on the Senegalese continental margin in the tropical North Atlantic Ocean: Insights from iron isotopes. Geochimica Et Cosmochimica Acta. https://doi.org/10.1016/j.gca.2018.02.031 <https://doi.org/10.1016/j.gca.2018.02.031> |
op_rights |
cc_by_nc_nd_4 |
op_rightsnorm |
CC-BY-NC-ND |
op_doi |
https://doi.org/10.1016/j.gca.2018.02.031 |
container_title |
Geochimica et Cosmochimica Acta |
container_volume |
236 |
container_start_page |
60 |
op_container_end_page |
78 |
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1766122324599242752 |