Average fluorescence and dissolved iron and Fe-binding ligand characteristics during POLARSTERN expedition ANT-XXIV/3 in 2008 ...

Organic complexation of dissolved iron (dFe) was investigated in the Atlantic sector of the Southern Ocean in order to understand the distribution of Fe over the whole water column. The total concentration of dissolved organic ligands ([Lt]) measured by voltammetry ranged between 0.54 and 1.84 nEq o...

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Main Authors: Thuróczy, Charles-Edouard, Gerringa, Loes J A, Klunder, Maarten B, Laan, Patrick, de Baar, Hein J W
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2011
Subjects:
IPY
Online Access:https://dx.doi.org/10.1594/pangaea.839219
https://doi.pangaea.de/10.1594/PANGAEA.839219
id ftdatacite:10.1594/pangaea.839219
record_format openpolar
spelling ftdatacite:10.1594/pangaea.839219 2024-09-15T18:14:50+00:00 Average fluorescence and dissolved iron and Fe-binding ligand characteristics during POLARSTERN expedition ANT-XXIV/3 in 2008 ... Thuróczy, Charles-Edouard Gerringa, Loes J A Klunder, Maarten B Laan, Patrick de Baar, Hein J W 2011 application/zip https://dx.doi.org/10.1594/pangaea.839219 https://doi.pangaea.de/10.1594/PANGAEA.839219 en eng PANGAEA https://dx.doi.org/10.1016/j.dsr2.2011.01.002 https://dx.doi.org/10.1016/j.dsr2.2010.10.042 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 International Polar Year 2007-2008 IPY article Collection Supplementary Publication Series of Datasets 2011 ftdatacite https://doi.org/10.1594/pangaea.83921910.1016/j.dsr2.2011.01.00210.1016/j.dsr2.2010.10.042 2024-08-01T10:52:43Z Organic complexation of dissolved iron (dFe) was investigated in the Atlantic sector of the Southern Ocean in order to understand the distribution of Fe over the whole water column. The total concentration of dissolved organic ligands ([Lt]) measured by voltammetry ranged between 0.54 and 1.84 nEq of M Fe whereas the conditional binding strength (K') ranged between 10**21.4 and 10**22.8. For the first time, trends in Fe-organic complexation were observed in an ocean basin by examining the ratio ([Lt]/[dFe]), defined as the organic ligand concentration divided by the dissolved Fe concentration. The [Lt]/[dFe] ratio indicates the saturation state of the natural ligands with Fe; a ratio near 1 means saturation of the ligands leading to precipitation of Fe. Reversely, high ratios mean Fe depletion and show a high potential for Fe solubilisation. In surface waters where phytoplankton is present low dissolved Fe and high variable ligand concentrations were found. Here the [Lt]/[dFe] ratio was on average 4.4. It ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... Article in Journal/Newspaper International Polar Year IPY Southern Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic International Polar Year 2007-2008 IPY
spellingShingle International Polar Year 2007-2008 IPY
Thuróczy, Charles-Edouard
Gerringa, Loes J A
Klunder, Maarten B
Laan, Patrick
de Baar, Hein J W
Average fluorescence and dissolved iron and Fe-binding ligand characteristics during POLARSTERN expedition ANT-XXIV/3 in 2008 ...
topic_facet International Polar Year 2007-2008 IPY
description Organic complexation of dissolved iron (dFe) was investigated in the Atlantic sector of the Southern Ocean in order to understand the distribution of Fe over the whole water column. The total concentration of dissolved organic ligands ([Lt]) measured by voltammetry ranged between 0.54 and 1.84 nEq of M Fe whereas the conditional binding strength (K') ranged between 10**21.4 and 10**22.8. For the first time, trends in Fe-organic complexation were observed in an ocean basin by examining the ratio ([Lt]/[dFe]), defined as the organic ligand concentration divided by the dissolved Fe concentration. The [Lt]/[dFe] ratio indicates the saturation state of the natural ligands with Fe; a ratio near 1 means saturation of the ligands leading to precipitation of Fe. Reversely, high ratios mean Fe depletion and show a high potential for Fe solubilisation. In surface waters where phytoplankton is present low dissolved Fe and high variable ligand concentrations were found. Here the [Lt]/[dFe] ratio was on average 4.4. It ... : Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ...
format Article in Journal/Newspaper
author Thuróczy, Charles-Edouard
Gerringa, Loes J A
Klunder, Maarten B
Laan, Patrick
de Baar, Hein J W
author_facet Thuróczy, Charles-Edouard
Gerringa, Loes J A
Klunder, Maarten B
Laan, Patrick
de Baar, Hein J W
author_sort Thuróczy, Charles-Edouard
title Average fluorescence and dissolved iron and Fe-binding ligand characteristics during POLARSTERN expedition ANT-XXIV/3 in 2008 ...
title_short Average fluorescence and dissolved iron and Fe-binding ligand characteristics during POLARSTERN expedition ANT-XXIV/3 in 2008 ...
title_full Average fluorescence and dissolved iron and Fe-binding ligand characteristics during POLARSTERN expedition ANT-XXIV/3 in 2008 ...
title_fullStr Average fluorescence and dissolved iron and Fe-binding ligand characteristics during POLARSTERN expedition ANT-XXIV/3 in 2008 ...
title_full_unstemmed Average fluorescence and dissolved iron and Fe-binding ligand characteristics during POLARSTERN expedition ANT-XXIV/3 in 2008 ...
title_sort average fluorescence and dissolved iron and fe-binding ligand characteristics during polarstern expedition ant-xxiv/3 in 2008 ...
publisher PANGAEA
publishDate 2011
url https://dx.doi.org/10.1594/pangaea.839219
https://doi.pangaea.de/10.1594/PANGAEA.839219
genre International Polar Year
IPY
Southern Ocean
genre_facet International Polar Year
IPY
Southern Ocean
op_relation https://dx.doi.org/10.1016/j.dsr2.2011.01.002
https://dx.doi.org/10.1016/j.dsr2.2010.10.042
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.83921910.1016/j.dsr2.2011.01.00210.1016/j.dsr2.2010.10.042
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