Massive Southern Ocean phytoplankton bloom fed by iron of possible hydrothermal origin.

Primary production in the Southern Ocean (SO) is limited by iron availability. Hydrothermal vents have been identified as a potentially important source of iron to SO surface waters. Here we identify a recurring phytoplankton bloom in the high-nutrient, low-chlorophyll waters of the Antarctic Circumpolar Current in the Pacific sector of the SO, that we argue is fed by iron of hydrothermal origin.

Massive difference in synonymous substitution rates among mitochondrial, plastid, and nuclear genes of Phaeocystis algae.

We are just beginning to understand how mutation rates differ among mitochondrial, plastid, and nuclear genomes. In most seed plants the mitochondrial mutation rate is estimated to be lower than those of the plastid and nucleus, whereas in the red alga Porphyra the opposite is true, and in certain green algae all three genomes appear to have similar rates of mutation. Relative rate statistics of organelle vs nuclear genes, however, are lacking for lineages that acquired their plastids through secondary endosymbiosis, but recent organelle DNA analyses suggest that they may differ drastically from what is observed in lineages with primary plastids, such as green plants and red algae.

Photophysiology in two major southern ocean phytoplankton taxa: photosynthesis and growth of Phaeocystis antarctica and Fragilariopsis cylindrus under different irradiance levels.

The Ross Sea, Antarctica, supports two distinct populations of phytoplankton, one that grows well in sea ice and blooms in the shallow mixed layers of the Western marginal ice zone and the other that can be found in sea ice but thrives in the deeply mixed layers of the Ross Sea. Dominated by diatoms (e.g.

Characterization of marine bacteria and the activity of their enzyme systems involved in degradation of the algal storage glucan laminarin.

The algal storage glucan laminarin is one of the most abundant carbon sources for marine prokaryotes. Its degradation was investigated in bacteria isolated during and after a spring phytoplankton bloom in the coastal North Sea. On average, 13% of prokaryotes detected by epifluorescence counts were able to grow in Most Probable Number dilution series on laminarin as sole carbon source.