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      Spatial patterns in phytoplankton biomass and pigment distributions in the Ross Sea

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      Journal of Geophysical Research: Oceans
      American Geophysical Union (AGU)

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          Importance of iron for plankton blooms and carbon dioxide drawdown in the Southern Ocean

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            Iron deficiency limits phytoplankton growth in Antarctic waters

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              Phytoplankton bloom produced by a receding ice edge in the ross sea: spatial coherence with the density field.

              Measurements of chlorophyll, particulate carbon, and biogenic silica concentrations near a receding ice edge off the coast of Victoria Land, Antarctica, indicated the presence of a dense phytoplankton bloom. The bloom extended 250 kilometers from the ice edge and was restricted to waters where the melting of ice had resulted in reduced salinity. The region involved was one of enhanced vertical stability, which may have favored phytoplankton growth, accumulation, or both. Epontic algae released from melting ice may have served as an inoculum for the bloom. Ratios of organic carbon to chlorophyll and biogenic silica to carbon were unusually high, resulting in high biogenic silica concentrations despite only moderately high chlorophyll levels.
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                Author and article information

                Journal
                Journal of Geophysical Research: Oceans
                J. Geophys. Res.
                American Geophysical Union (AGU)
                01480227
                August 15 1996
                August 15 1996
                : 101
                : C8
                : 18467-18477
                Article
                10.1029/96JC00034
                a9aa2383-cb7b-41d8-bd97-bd3085221c1e
                © 1996

                http://doi.wiley.com/10.1002/tdm_license_1.1

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