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Sea ice and oceanic boundaries have a dominant effect in structuring Antarctic
marine ecosystems. Satellite imagery and historical data have identified the
southern boundary of the Antarctic Circumpolar Current as a
site of enhanced biological productivity. Meso-scale surveys
off the Antarctic peninsula have related the abundances of Antarctic krill
(Euphausia superba) and salps (Salpa thompsoni) to inter-annual
variations in sea-ice extent. Here we have examined the ecosystem
structure and oceanography spanning 3,500 km of the east Antarctic
coastline, linking the scales of local surveys and global observations. Between
80° and 150° E there is a threefold variation in the extent
of annual sea-ice cover, enabling us to examine the regional effects of sea
ice and ocean circulation on biological productivity. Phytoplankton, primary
productivity, Antarctic krill, whales and seabirds were concentrated where
winter sea-ice extent is maximal, whereas salps were located where the sea-ice
extent is minimal. We found enhanced biological activity south of the southern
boundary of the Antarctic Circumpolar Current rather than in association with
it. We propose that along this coastline ocean circulation
determines both the sea-ice conditions and the level of biological productivity
at all trophic levels.