Distinct profiles of size-fractionated iron-binding ligands between the eastern and western subarctic Pacific

Abstract Iron (Fe) is well known as a limiting factor to control primary productivity especially in high-nutrient and low chlorophyll area such as the subarctic Pacific. The solubility of Fe is believed to be controlled by its complexation with natural organic ligands, while the distribution of orga...

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Main Authors: Yoshiko Kondo, Rise Bamba, Hajime Obata, Jun Nishioka, Shigenobu Takeda
Format: Article
Language:English
Published: Nature Publishing Group 2021-01-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-81536-6
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spelling doaj-95ed7869e4e04bf49a11c6cf2e6ea1f72021-01-24T12:29:35ZengNature Publishing GroupScientific Reports2045-23222021-01-011111910.1038/s41598-021-81536-6Distinct profiles of size-fractionated iron-binding ligands between the eastern and western subarctic PacificYoshiko Kondo0Rise Bamba1Hajime Obata2Jun Nishioka3Shigenobu Takeda4Graduate School of Fisheries and Environmental Sciences, Nagasaki UniversityPan-Okhotsk Research Center, Institute of Low Temperature Science, Hokkaido UniversityAtmosphere and Ocean Research Institute, The University of TokyoPan-Okhotsk Research Center, Institute of Low Temperature Science, Hokkaido UniversityGraduate School of Fisheries and Environmental Sciences, Nagasaki UniversityAbstract Iron (Fe) is well known as a limiting factor to control primary productivity especially in high-nutrient and low chlorophyll area such as the subarctic Pacific. The solubility of Fe is believed to be controlled by its complexation with natural organic ligands, while the distribution of organic ligands is poorly understood. Here, we report that dissolved (< 0.2 µm) organic ligands were unevenly distributed between the western and eastern stations in the subarctic Pacific. The concentration of dissolved organic ligands around the lower part of subarctic Pacific intermediate water was higher in the western station, suggesting that Fe complexation with these organic ligands supports a lateral transport within the water mass. However, a more detailed size-fractionated treatment indicated no significant difference in the soluble (< 1000 kDa) ligands’ distribution between the western and eastern stations. These results suggest that organic and inorganic colloid formations are potentially essential for Fe transport mechanisms in the subarctic Pacific.https://doi.org/10.1038/s41598-021-81536-6
collection DOAJ
language English
format Article
sources DOAJ
author Yoshiko Kondo
Rise Bamba
Hajime Obata
Jun Nishioka
Shigenobu Takeda
spellingShingle Yoshiko Kondo
Rise Bamba
Hajime Obata
Jun Nishioka
Shigenobu Takeda
Distinct profiles of size-fractionated iron-binding ligands between the eastern and western subarctic Pacific
Scientific Reports
author_facet Yoshiko Kondo
Rise Bamba
Hajime Obata
Jun Nishioka
Shigenobu Takeda
author_sort Yoshiko Kondo
title Distinct profiles of size-fractionated iron-binding ligands between the eastern and western subarctic Pacific
title_short Distinct profiles of size-fractionated iron-binding ligands between the eastern and western subarctic Pacific
title_full Distinct profiles of size-fractionated iron-binding ligands between the eastern and western subarctic Pacific
title_fullStr Distinct profiles of size-fractionated iron-binding ligands between the eastern and western subarctic Pacific
title_full_unstemmed Distinct profiles of size-fractionated iron-binding ligands between the eastern and western subarctic Pacific
title_sort distinct profiles of size-fractionated iron-binding ligands between the eastern and western subarctic pacific
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2021-01-01
description Abstract Iron (Fe) is well known as a limiting factor to control primary productivity especially in high-nutrient and low chlorophyll area such as the subarctic Pacific. The solubility of Fe is believed to be controlled by its complexation with natural organic ligands, while the distribution of organic ligands is poorly understood. Here, we report that dissolved (< 0.2 µm) organic ligands were unevenly distributed between the western and eastern stations in the subarctic Pacific. The concentration of dissolved organic ligands around the lower part of subarctic Pacific intermediate water was higher in the western station, suggesting that Fe complexation with these organic ligands supports a lateral transport within the water mass. However, a more detailed size-fractionated treatment indicated no significant difference in the soluble (< 1000 kDa) ligands’ distribution between the western and eastern stations. These results suggest that organic and inorganic colloid formations are potentially essential for Fe transport mechanisms in the subarctic Pacific.
url https://doi.org/10.1038/s41598-021-81536-6
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