Articles | Volume 18, issue 15
https://doi.org/10.5194/bg-18-4587-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-18-4587-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
11 Aug 2021
Research article |
| 11 Aug 2021
| 11 Aug 2021
Fe-binding organic ligands in coastal and frontal regions of the western Antarctic Peninsula
Indah Ardiningsih
CORRESPONDING AUTHOR
Department of Ocean Systems, NIOZ Royal Netherlands Institute for Sea Research and Utrecht University, Texel, 1797SH, the
Netherlands
Kyyas Seyitmuhammedov
Centre for Trace Element Analysis and Chemistry Department, University
of Otago, Dunedin, New Zealand
Sylvia G. Sander
International Atomic Energy Agency, 4a Quai Antoine 1er, 98000,
Principality of Monaco, Monaco
Claudine H. Stirling
Centre for Trace Element Analysis and Chemistry Department, University
of Otago, Dunedin, New Zealand
Gert-Jan Reichart
Department of Ocean Systems, NIOZ Royal Netherlands Institute for Sea Research and Utrecht University, Texel, 1797SH, the
Netherlands
Faculty of Geosciences, Earth Sciences Department, Utrecht University, Utrecht, 3512JE, the
Netherlands
Kevin R. Arrigo
Department of Earth System Science, Stanford University, USA
Loes J. A. Gerringa
Department of Ocean Systems, NIOZ Royal Netherlands Institute for Sea Research and Utrecht University, Texel, 1797SH, the
Netherlands
Rob Middag
Department of Ocean Systems, NIOZ Royal Netherlands Institute for Sea Research and Utrecht University, Texel, 1797SH, the
Netherlands
Centre for Trace Element Analysis and Chemistry Department, University
of Otago, Dunedin, New Zealand
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- Trace metals in natural lakes: seasonal variation of manganese, cobalt, nickel, copper and zinc speciation in lakes of different trophic states M. Dengg et al. 10.1007/s10533-024-01207-2
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- Distribution of dissolved aluminum and dissolved iron in Kongsfjorden: A glacial fjord in the Arctic Z. Shen et al. 10.1016/j.marchem.2024.104399
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- A proposed seasonal cycle of dissolved iron-binding ligands in Antarctic sea ice C. Genovese et al. 10.1525/elementa.2021.00030
10 citations as recorded by crossref.
- Atmospheric Iron and Aluminium Deposition and Sea-Surface Dissolved Iron and Aluminium Concentrations in the South China Sea off Malaysia Borneo (Sarawak Waters) F. Idrus et al. 10.33736/bjrst.4166.2021
- The distribution of Fe across the shelf of the Western Antarctic Peninsula at the start of the phytoplankton growing season K. Seyitmuhammedov et al. 10.1016/j.marchem.2021.104066
- Trace metals in natural lakes: seasonal variation of manganese, cobalt, nickel, copper and zinc speciation in lakes of different trophic states M. Dengg et al. 10.1007/s10533-024-01207-2
- Trace Element (Fe, Co, Ni and Cu) Dynamics Across the Salinity Gradient in Arctic and Antarctic Glacier Fjords J. Krause et al. 10.3389/feart.2021.725279
- Seasonal dispersal of fjord meltwaters as an important source of iron and manganese to coastal Antarctic phytoplankton K. Forsch et al. 10.5194/bg-18-6349-2021
- Potential interactions between diatoms and bacteria are shaped by trace element gradients in the Southern Ocean A. Sterling et al. 10.3389/fmars.2022.876830
- Cycling and behavior of 230Th in the Arctic Ocean: Insights from sedimentary archives T. Song et al. 10.1016/j.earscirev.2023.104514
- Identifying potential sources of iron-binding ligands in coastal Antarctic environments and the wider Southern Ocean A. Smith et al. 10.3389/fmars.2022.948772
- Distribution of dissolved aluminum and dissolved iron in Kongsfjorden: A glacial fjord in the Arctic Z. Shen et al. 10.1016/j.marchem.2024.104399
- The Distribution of Dissolved Copper and Natural Organic Ligands in Tropical Coastal Waters Under Seasonal Variation L. Ng et al. 10.3390/jmse13030446
1 citations as recorded by crossref.
Latest update: 29 Jul 2025
Short summary
Organic Fe speciation is investigated along a natural gradient of the western Antarctic Peninsula from an ice-covered shelf to the open ocean. The two major fronts in the region affect the distribution of ligands. The excess ligands not bound to dissolved Fe (DFe) comprised up to 80 % of the total ligand concentrations, implying the potential to solubilize additional Fe input. The ligands on the shelf can increase the DFe residence time and fuel local primary production upon ice melt.
Organic Fe speciation is investigated along a natural gradient of the western Antarctic...
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