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The fugacity of CO 2 and abundance of chlorophyll a (Chla) were determined in two long transects from the Polar Front to the Antarctic Continent in austral summer, December 1995-January 1996. Large undersaturations of CO 2 in the surface water were observed coinciding with high Chla content. In the major hydrographic regions the mean air-sea fluxes were found to range from -3 to +7mmolm...
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