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The concept that organlc carbon IS transported to the equatorial region at in termed~ate water depths from subantarct~c frontal zones has been r e -~nves t~ga ted uslng the tri t~ated thym~dlne method to determine rates of bactenal DNA synthes~s in water masses of the Tasman Sea There was a higher bactenal growth rate and thus a h ~ g h e r flux of organlc carbon through bactena in the Antarctic Intermediate Water (900 to 1000 m depth) than In the water masses immediately above or below In the Tasman Sea east and south of Tasman~a Values for bactenal production were 4 to 8 pg C m-3 dl , whlch are equivalent to a consumptlon of about 3 to 6 p1 0, I ' yr.' In the deeper layer at 1200 to 1500 m rates were 3 to 4 times lower These rates are coinpat~ble with other data on oxygen utllisat~on Our results support the concept that organic matter slnks ~11th downwelhng water In the zone between the Subtropical Convergence and the Polar Front in the Southern Ocean and 15 advected towards the equator below the photlc zone

Organic carbon transport from the Southern Ocean and bacterial growth in the Antarctic intermediate Water masses of the Tasman Sea