The late stage of the North East Atlantic (NEA) spring bloom was investigated during June 2005 along a transect section from 45 to 66° N between 15 and 20° W in order to characterize the contribution of siliceous and calcareous phytoplankton groups and describe their distribution in relation to environmental factors. We measured several biogeochemical parameters such as nutrients, surface trace metals, algal pigments, biogenic silica (BSi), particulate inorganic carbon (PIC) or calcium carbonate, particulate organic carbon, nitrogen and phosphorus (POC, PON and POP, respectively), as well as transparent exopolymer particles (TEP). Results were compared with other studies undertaken in this area since the JGOFS NABE program. Characteristics ...
The North Atlantic is characterized by diatom-dominated spring blooms that results in significant tr...
The duration and magnitude of the North Atlantic spring bloom impacts both higher trophic levels and...
A full understanding of the biogeochemical cycling of silica in the North Atlantic is hampered by a ...
The late stage of the North East Atlantic (NEA) spring bloom was investigated during June 2005 along...
We determined the spatial and temporal dynamics of major phytoplankton groups in relation to biogeoc...
International audienceThe Si cycle in the northeast Atlantic (40°–43.5°N, 15°–21°W) was investigated...
During the North Atlantic spring bloom, a seasonal phytoplankton community succession takes place fr...
Diatoms are generally the dominant contributors to the Arctic Ocean spring bloom, which is a key eve...
Vertical distributions of biogenic silica (bSi), particulate inorganic carbon (PIC) and key biominer...
The spring bloom is a key annual event in the phenology of pelagic ecosystems, making a major contri...
The standing stocks and production rates of particulate organic carbon (POC) and biogenic silica (bS...
The North Atlantic is characterized by diatom-dominated spring blooms that results in significant tr...
The duration and magnitude of the North Atlantic spring bloom impacts both higher trophic levels and...
A full understanding of the biogeochemical cycling of silica in the North Atlantic is hampered by a ...
The late stage of the North East Atlantic (NEA) spring bloom was investigated during June 2005 along...
We determined the spatial and temporal dynamics of major phytoplankton groups in relation to biogeoc...
International audienceThe Si cycle in the northeast Atlantic (40°–43.5°N, 15°–21°W) was investigated...
During the North Atlantic spring bloom, a seasonal phytoplankton community succession takes place fr...
Diatoms are generally the dominant contributors to the Arctic Ocean spring bloom, which is a key eve...
Vertical distributions of biogenic silica (bSi), particulate inorganic carbon (PIC) and key biominer...
The spring bloom is a key annual event in the phenology of pelagic ecosystems, making a major contri...
The standing stocks and production rates of particulate organic carbon (POC) and biogenic silica (bS...
The North Atlantic is characterized by diatom-dominated spring blooms that results in significant tr...
The duration and magnitude of the North Atlantic spring bloom impacts both higher trophic levels and...
A full understanding of the biogeochemical cycling of silica in the North Atlantic is hampered by a ...