The availability of iron (Fe) to marine microbial communities is enhanced through complexation by ligands. In Fe limited environments, measuring the distribution and identifying the likely sources of ligands is therefore central to understanding the drivers of marine productivity. Antarctic coastal marine environments support highly productive ecosystems and are influenced by numerous sources of ligands, the magnitude of which varies both spatially and seasonally. Using competitive ligand exchange adsorptive cathodic stripping voltammetry (CLE-AdCSV) with 2-(2-thiazolylazo)-p-cresol (TAC) as a competing artificial ligand, this study investigates Fe-binding ligands (FeL) across the continental shelf break in the Mertz Glacier Region, East An...
Organic complexation of dissolved iron (dFe) was investigated in the Atlantic sector of the Southern...
International audienceDuring the Kerguelen Ocean and Plateau compared Study (KEOPS; January–February...
International audienceDissolved iron (dFe) availability limits the uptake of atmospheric CO 2 by the...
Organic ligands are a key factor determining the availability of dissolved iron (DFe) in the high-nu...
Organic ligands determine the threshold of dissolved-Fe (DFe) concentrations in seawater. Understand...
Recent years have seen an increased occurrence of large icebergs in the Southern Ocean originating f...
Despite widespread iron (Fe) limitation in the Southern Ocean, Antarctic coastlines are highly produ...
The Ross Sea Polynya (RSP) has the highest primary production of Antarctic waters. Iron (Fe) is one ...
Since Antarctic sea ice covers an area larger than the Antarctic continent itself, the discovery tha...
Iron (Fe) is the limiting nutrient for primary productivity in the Southern Ocean, with much of the ...
The availability of iron (Fe) is decisive for biochemical reactions involved in marine primary produ...
Primary productivity in the Amundsen Sea (Southern Ocean) is among the highest in Antarctica. The su...
Organic complexation of dissolved iron (dFe) was investigated in the Atlantic sector of the Southern...
International audienceDuring the Kerguelen Ocean and Plateau compared Study (KEOPS; January–February...
International audienceDissolved iron (dFe) availability limits the uptake of atmospheric CO 2 by the...
Organic ligands are a key factor determining the availability of dissolved iron (DFe) in the high-nu...
Organic ligands determine the threshold of dissolved-Fe (DFe) concentrations in seawater. Understand...
Recent years have seen an increased occurrence of large icebergs in the Southern Ocean originating f...
Despite widespread iron (Fe) limitation in the Southern Ocean, Antarctic coastlines are highly produ...
The Ross Sea Polynya (RSP) has the highest primary production of Antarctic waters. Iron (Fe) is one ...
Since Antarctic sea ice covers an area larger than the Antarctic continent itself, the discovery tha...
Iron (Fe) is the limiting nutrient for primary productivity in the Southern Ocean, with much of the ...
The availability of iron (Fe) is decisive for biochemical reactions involved in marine primary produ...
Primary productivity in the Amundsen Sea (Southern Ocean) is among the highest in Antarctica. The su...
Organic complexation of dissolved iron (dFe) was investigated in the Atlantic sector of the Southern...
International audienceDuring the Kerguelen Ocean and Plateau compared Study (KEOPS; January–February...
International audienceDissolved iron (dFe) availability limits the uptake of atmospheric CO 2 by the...