Abstract
The year 2014 is between one of the coldest La Niña events (2011−2012), and one of the most intense warming events between (2013–2016) in the California Current System (CCS). The information provided in this work documents part of the missing information about zooplankton and oceanographic features for the year 2014 along the southern portion of the CCS off the western Coast of Baja California Peninsula (WBCP). The statistical analysis of environmental variables during the summer of 2014 distinguished three regions off the WBCP (north, transitional, and south), in coincidence with changes in zooplankton groups composition. Thermal and saline oceanic fronts off the central region coincided with an increasing abundance of gelatinous zooplankton, where two cold core eddies were present. These mesoscale structures represent physical barriers that seem to determine the distribution limits of planktonic communities. Since no day/night statistical differences in zooplankton composition were found, zooplankton community changes seem more related to the latitudinal environmental changes and mesoscale semi-permanent structures in the middle peninsula.
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