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Zooplankton data collected during September 1995 in the North West Atlantic at 41°39'N, 49°58'W (the location of the site of the 'Titanic' wreck) were analysed. The region investigated was characterized by a very sharp frontal zone between the Gulf Stream and the main stream of the Labrador Current. The total plankton biomass in the water column was very high. The macroplank- ton biomass values below the 600 m layer were significantly higher as compared with the similar values measured before in other productive boreal regions of the Atlantic and Pacific oceans. A lot of dead mesoplankton animals occurred in the deep layers. The reason was that the cold-water mesoplank- ton advected by the Labrador Current died off intensively within the deep layers of the frontal zone and were used as a food resource by the macroplankton carnivores and scavengers that were very abundant there.

Vertical distribution of zooplankton in the frontal zone of the Gulf Stream and Labrador Current