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      The overwintering strategy of Antarctic krill under the pack-ice of the Weddell Sea

      Polar Biology
      Springer Nature

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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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            Seals and Whales of the Southern Ocean

            R. Laws (1977)
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              A physical mechanism for establishing algal populations in frazil ice

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                Author and article information

                Journal
                Polar Biology
                Polar Biol
                Springer Nature
                0722-4060
                1432-2056
                December 1988
                December 1988
                : 9
                : 2
                : 129-135
                Article
                10.1007/BF00442041
                8d3ebae2-f2c2-4d72-900d-d7d20d817646
                © 1988
                History

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