The distribution of dissolved iron and its chemical speciation (organic complexation and redox speciation) were studied in the northeastern Atlantic Ocean along 23°W between 37 and 42°N at depths between 0 and 2000 m, and in the upper-water column (upper 200 m) at two stations further east at 45°N10°W and 40°N17°W in the early spring of 1998. The iron speciation data are here combined with phytoplankton data to suggest cyanobacteria as a possible source for the iron binding ligands. The organic Fe-binding ligand concentrations were greater than that of dissolved iron by a factor of 1.5–5, thus maintaining iron in solution at levels well above it solubility. The water column distribution of the organic ligand indicates in-situ production of ...
To investigate the biogeochemistry of iron in the waters of the European continental margin, we dete...
It is now well established that Iron (Fe) is a limiting element in many regions of the open ocean. O...
Variations in the speciation of iron in the northern North Sea were investigated in an area covering...
The distribution of dissolved iron and its chemical speciation (organic complexation and redox speci...
A transect across the eastern North Atlantic from 42°N, 23°W towards the European continental shelf ...
The chemical speciation of iron was determined in the Southern Ocean along a transect from 48 to 70°...
Organic complexation of dissolved iron (dFe) was investigated in the Atlantic sector of the Southern...
The chemical speciation of iron was determined in the Southern Ocean along a transect from 48 to 703...
It is now recognized that iron (Fe) availability dictates the efficiency of the global biological ca...
The characteristics of the dissolved iron (DFe) binding organic ligands were determined during 3 Dut...
In the Eastern North Atlantic Ocean iron (Fe) speciation was investigated in three size fractions th...
On voyages in the Iceland Basin in 2007 and 2009, we observed low (ca. 0.1 nM) total dissolved iron ...
Iron (Fe) is an essential micronutrient for marine organisms, and it is now well established that lo...
Iron (Fe) is an essential micronutrient for marine organisms, and it is now well established that lo...
Organic complexation of dissolved iron (dFe) was investigated in the Atlantic sector of the Southern...
To investigate the biogeochemistry of iron in the waters of the European continental margin, we dete...
It is now well established that Iron (Fe) is a limiting element in many regions of the open ocean. O...
Variations in the speciation of iron in the northern North Sea were investigated in an area covering...
The distribution of dissolved iron and its chemical speciation (organic complexation and redox speci...
A transect across the eastern North Atlantic from 42°N, 23°W towards the European continental shelf ...
The chemical speciation of iron was determined in the Southern Ocean along a transect from 48 to 70°...
Organic complexation of dissolved iron (dFe) was investigated in the Atlantic sector of the Southern...
The chemical speciation of iron was determined in the Southern Ocean along a transect from 48 to 703...
It is now recognized that iron (Fe) availability dictates the efficiency of the global biological ca...
The characteristics of the dissolved iron (DFe) binding organic ligands were determined during 3 Dut...
In the Eastern North Atlantic Ocean iron (Fe) speciation was investigated in three size fractions th...
On voyages in the Iceland Basin in 2007 and 2009, we observed low (ca. 0.1 nM) total dissolved iron ...
Iron (Fe) is an essential micronutrient for marine organisms, and it is now well established that lo...
Iron (Fe) is an essential micronutrient for marine organisms, and it is now well established that lo...
Organic complexation of dissolved iron (dFe) was investigated in the Atlantic sector of the Southern...
To investigate the biogeochemistry of iron in the waters of the European continental margin, we dete...
It is now well established that Iron (Fe) is a limiting element in many regions of the open ocean. O...
Variations in the speciation of iron in the northern North Sea were investigated in an area covering...