The Physicochemical Speciation of Dissolved Iron in the Bering Sea, Alaska

The physicochemical speciation of dissolved iron (Fe) across natural dissolved Fe gradients in the oceanic and shelf domains of the southeastern Bering Sea was examined in surface and subsurface samples using competitive ligand exchange‐adsorptive cathodic stripping voltammetry with the added ligand...

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Published in:Limnology and Oceanography
Main Authors: Buck, Kristen N., Bruland, Kenneth W.
Format: Article in Journal/Newspaper
Language:unknown
Published: Digital Commons @ University of South Florida 2007
Subjects:
Online Access:https://digitalcommons.usf.edu/msc_facpub/620
https://doi.org/10.4319/lo.2007.52.5.1800
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spelling ftusouthflorida:oai:digitalcommons.usf.edu:msc_facpub-1618 2023-07-30T04:02:40+02:00 The Physicochemical Speciation of Dissolved Iron in the Bering Sea, Alaska Buck, Kristen N. Bruland, Kenneth W. 2007-09-27T07:00:00Z https://digitalcommons.usf.edu/msc_facpub/620 https://doi.org/10.4319/lo.2007.52.5.1800 unknown Digital Commons @ University of South Florida https://digitalcommons.usf.edu/msc_facpub/620 doi:10.4319/lo.2007.52.5.1800 https://doi.org/10.4319/lo.2007.52.5.1800 Marine Science Faculty Publications Life Sciences article 2007 ftusouthflorida https://doi.org/10.4319/lo.2007.52.5.1800 2023-07-13T20:45:14Z The physicochemical speciation of dissolved iron (Fe) across natural dissolved Fe gradients in the oceanic and shelf domains of the southeastern Bering Sea was examined in surface and subsurface samples using competitive ligand exchange‐adsorptive cathodic stripping voltammetry with the added ligand salicylaldoxime. Two ligand classes were measured in all samples, a stronger L1 ligand class and a weaker L2 ligand class. Conditional stability constants for both ligand classes were comparable between surface and subsurface samples, with mean log KcondFeL1,Fe0 = 11.5 ± 0.3 and mean log KcondFeL2,Fe0 = 10.3 ± 0.3 in surface samples, and mean log KcondFeL1,Fe0 = 11.4 ± 0.2 with a weaker ligand and mean log KcondFeL2,Fe0 of 10.2 ± 0.2 in subsurface samples. The concentrations of dissolved Fe were strongly correlated with ambient stronger L1 ligand concentrations for all samples with dissolved Fe concentrations greater than 0.2 nmol L−1. In samples with dissolved Fe concentrations less than 0.2 nmol L−1, large and variable excesses of L1 ligand concentrations were measured, coincident with observed Fe stress or limitation on the ambient phytoplankton. These observations suggest that the phytoplankton community is readily able to access dissolved Fe from the FeL1 complex, resulting in excess L1 in these waters. The available speciation data from other sources indicate that a significant correlation exists between dissolved Fe and L1 ligand concentrations in samples with intermediate dissolved Fe, and this is a seemingly ubiquitous feature of dissolved Fe cycling in the marine environment. Article in Journal/Newspaper Bering Sea Alaska University of South Florida St. Petersburg: Digital USFSP Bering Sea Limnology and Oceanography 52 5 1800 1808
institution Open Polar
collection University of South Florida St. Petersburg: Digital USFSP
op_collection_id ftusouthflorida
language unknown
topic Life Sciences
spellingShingle Life Sciences
Buck, Kristen N.
Bruland, Kenneth W.
The Physicochemical Speciation of Dissolved Iron in the Bering Sea, Alaska
topic_facet Life Sciences
description The physicochemical speciation of dissolved iron (Fe) across natural dissolved Fe gradients in the oceanic and shelf domains of the southeastern Bering Sea was examined in surface and subsurface samples using competitive ligand exchange‐adsorptive cathodic stripping voltammetry with the added ligand salicylaldoxime. Two ligand classes were measured in all samples, a stronger L1 ligand class and a weaker L2 ligand class. Conditional stability constants for both ligand classes were comparable between surface and subsurface samples, with mean log KcondFeL1,Fe0 = 11.5 ± 0.3 and mean log KcondFeL2,Fe0 = 10.3 ± 0.3 in surface samples, and mean log KcondFeL1,Fe0 = 11.4 ± 0.2 with a weaker ligand and mean log KcondFeL2,Fe0 of 10.2 ± 0.2 in subsurface samples. The concentrations of dissolved Fe were strongly correlated with ambient stronger L1 ligand concentrations for all samples with dissolved Fe concentrations greater than 0.2 nmol L−1. In samples with dissolved Fe concentrations less than 0.2 nmol L−1, large and variable excesses of L1 ligand concentrations were measured, coincident with observed Fe stress or limitation on the ambient phytoplankton. These observations suggest that the phytoplankton community is readily able to access dissolved Fe from the FeL1 complex, resulting in excess L1 in these waters. The available speciation data from other sources indicate that a significant correlation exists between dissolved Fe and L1 ligand concentrations in samples with intermediate dissolved Fe, and this is a seemingly ubiquitous feature of dissolved Fe cycling in the marine environment.
format Article in Journal/Newspaper
author Buck, Kristen N.
Bruland, Kenneth W.
author_facet Buck, Kristen N.
Bruland, Kenneth W.
author_sort Buck, Kristen N.
title The Physicochemical Speciation of Dissolved Iron in the Bering Sea, Alaska
title_short The Physicochemical Speciation of Dissolved Iron in the Bering Sea, Alaska
title_full The Physicochemical Speciation of Dissolved Iron in the Bering Sea, Alaska
title_fullStr The Physicochemical Speciation of Dissolved Iron in the Bering Sea, Alaska
title_full_unstemmed The Physicochemical Speciation of Dissolved Iron in the Bering Sea, Alaska
title_sort physicochemical speciation of dissolved iron in the bering sea, alaska
publisher Digital Commons @ University of South Florida
publishDate 2007
url https://digitalcommons.usf.edu/msc_facpub/620
https://doi.org/10.4319/lo.2007.52.5.1800
geographic Bering Sea
geographic_facet Bering Sea
genre Bering Sea
Alaska
genre_facet Bering Sea
Alaska
op_source Marine Science Faculty Publications
op_relation https://digitalcommons.usf.edu/msc_facpub/620
doi:10.4319/lo.2007.52.5.1800
https://doi.org/10.4319/lo.2007.52.5.1800
op_doi https://doi.org/10.4319/lo.2007.52.5.1800
container_title Limnology and Oceanography
container_volume 52
container_issue 5
container_start_page 1800
op_container_end_page 1808
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