Southern Ocean phytoplankton are especially subjected to pronounced seasonal and interannual changes in light availability. Although previous studies have examined the role of light in these environments, very few combined pigment-based taxonomy with flow cytometry to better discriminate the light response of various phytoplankton groups. In particular the different populations within the diverse and important taxonomic group of diatoms require further investigation. Six incubation experiments (9–10 days) were performed during the main productive period with natural seawater collected at the Western Antarctic Peninsula. Standing stock of Phaeocystis spp. cells displayed relatively fast accumulation under all levels of light (low, medium, hi...
The Western Antarctic Peninsula (WAP), one of the most productive regions of the Southern Ocean, is ...
Light and dissolved iron (dFe) availability control net primary production (NPP) in much of the Sout...
The photosynthetic parameters of natural phytoplankton assemblages from the Ross Sea, Antarctica, as...
Southern Ocean phytoplankton are especially subjected to pronounced seasonal and interannual changes...
Climate change at the Western Antarctic Peninsula (WAP) is predicted to cause major changes in phyto...
Climate change at the Western Antarctic Peninsula (WAP) is predicted to cause major changes in phyto...
Diatoms are one of the dominant groups in phytoplankton communities of the western Antarctic Peninsu...
The role of iron and light in controlling photosynthate production and allocation in phytoplankton p...
The composition and distribution of phytoplankton assemblages around the tip of the Antarctic Penins...
Coastal zones of Antarctica harbor rich but highly variable phytoplankton communities. The mechanism...
Although iron (Fe) availability sets primarily the rate of phytoplankton growth and primary and expo...
The effects of climate change, including ocean acidification (OA), on future Southern Ocean phytopla...
To study how natural Southern Ocean phytoplankton communities acclimate to rapid fluctuations in irr...
The effects of climate change, including ocean acidification (OA), on future Southern Ocean phytopla...
The Western Antarctic Peninsula (WAP), one of the most productive regions of the Southern Ocean, is ...
Light and dissolved iron (dFe) availability control net primary production (NPP) in much of the Sout...
The photosynthetic parameters of natural phytoplankton assemblages from the Ross Sea, Antarctica, as...
Southern Ocean phytoplankton are especially subjected to pronounced seasonal and interannual changes...
Climate change at the Western Antarctic Peninsula (WAP) is predicted to cause major changes in phyto...
Climate change at the Western Antarctic Peninsula (WAP) is predicted to cause major changes in phyto...
Diatoms are one of the dominant groups in phytoplankton communities of the western Antarctic Peninsu...
The role of iron and light in controlling photosynthate production and allocation in phytoplankton p...
The composition and distribution of phytoplankton assemblages around the tip of the Antarctic Penins...
Coastal zones of Antarctica harbor rich but highly variable phytoplankton communities. The mechanism...
Although iron (Fe) availability sets primarily the rate of phytoplankton growth and primary and expo...
The effects of climate change, including ocean acidification (OA), on future Southern Ocean phytopla...
To study how natural Southern Ocean phytoplankton communities acclimate to rapid fluctuations in irr...
The effects of climate change, including ocean acidification (OA), on future Southern Ocean phytopla...
The Western Antarctic Peninsula (WAP), one of the most productive regions of the Southern Ocean, is ...
Light and dissolved iron (dFe) availability control net primary production (NPP) in much of the Sout...
The photosynthetic parameters of natural phytoplankton assemblages from the Ross Sea, Antarctica, as...