Mesozooplankton abundance and physiological rates in copepods were measured at selected sites in the Alboran Sea, in May 1991, on Cruise Almofront 1 (JGofs-France). Higher total zooplankton standing stocks, higher copepod abundance, higher feeding activity by the latter and a higher proportion of phytoplankton-derived carbohydrates in their diet were found in the geostrophic jet of inflowing Atlantic water than in surrounding areas, which offered a range of oligotrophic conditions. Relationships with data obtained in other disciplinary fields on the same cruise show that biological enrichment was due to locally enhanced production rather than advection of exogenous living matter. In the most productive context, sustained production effected by phytoplankton cells in the > 10 μm class size (diatoms) was being significantly transferred to higher trophic levels through herbivores with a relatively long generation time (copepods). The processes responsible for the fertilization, and their relationship to the jet and its frontal boundary, are discussed.
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