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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2021-01-01
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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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