Zooplankton variability and possible oceanographic anomalies from 1996 to 2009 on the south coast of Brazil

Abstract

The analysis of 14 years of sampling data on the zooplankton community in southern Brazil showed a tendency toward increased density and reduced species richness. This behavior could be a response to a prolonged period of negative sea surface temperature (SST) anomalies in the Pacific Ocean and the ENSO phenomenon. The persistence of the La Niña phenomenon between 2001 and 2008 was associated with a higher incidence of stress from southwest winds and a greater reach of the front of the La Plata River plume, with possible responses being lower temperatures in the summer/autumn and lower salinities in the winter/spring in the study area. Under these conditions, one response in the zooplankton community was larger copepod domains. This group was responsible for specific changes in the community, with an increase in the population of Acartia tonsa while populations of species with more thermophilic characteristics showed a decrease. It cannot be disregarded, however, that possible interactions between different abiotic and biotic forces acting in the environment may have influenced the structure of the community. It remains unknown whether a new steady state has been established in the environment or whether there has been a return to initial conditions.

Key words
Decrease in regional salinity; front of the La Plata River plume; regional cooling; zooplanktonic alteration