The importance of small-sized copepods in a frontal area of the Aegean Sea

Distribution, production and grazing of the copepod communitywere investigated in the northern Aegean Sea, which is characterizedby a permanent thermohaline front. Cruises were conducted alonga transect crossing the frontal area during spring and latesummer. Biomass and production of autotrophs were measured bysize fractionation and heterotrophic nanoflagellates and ciliateswere also studied. Copepod biomass, production and grazing impacton the phytoplankton and ciliate populations were estimated.The copepod community was sampled with a 45 µm net toinclude the smallest species and their developmental stages.The size, structure and distribution of the phytoplankton implythat most carbon was fixed by picoplankton during both seasonsand throughout the study area. The partitioning of carbon amongthe different plankton compartments was not a broad-based pyramidand the biomass of heterotrophs was higher than that of autotrophs,except in the non-frontal region during spring. Copepod biomasswas substantially higher in the frontal area. Our results showedthat the small-sized copepods (calanoids and cyclopoids) dominatedin terms of biomass and production, but also had a greater influenceon the efficiency of the trophic coupling between the primaryproducers and the protozooplankton than the larger species,stressing their importance in the northern Aegean Sea and theEastern Mediterranean in general.     

Zooplankton distribution and diversity in a frontal area of the Aegean Sea

This study was carried out in the northern Aegean Sea during late summer and spring. The aim was to examine the spatial and temporal distribution of the zooplankton community across a dynamic frontal area and to investigate how the oceanographic heterogeneity structures the composition of the zooplankton assemblages. The low-salinity and cold Black Sea water coming from the Dardanelles Strait is modified by mixing with the underlying warm and saline Aegean water. These hydrological features result in a pronounced thermohaline front in the northern Aegean Sea throughout the year. In both seasons, zooplankton was collected using both 45 and 200 µm mesh plankton nets. A high abundance of zooplankton was observed in the surface layer at the stations closest to the Dardanelles Strait on the stratified side of the front. The zooplankton distribution and community structure in the northern Aegean Sea were strongly influenced by the hydrological features. The frontal structure acts as a boundary for the zooplankton community. The surface layer at the stratified stations had the lowest copepod diversity, from where it increased with depth and horizontally as the stratification weakened outside of the front. The total abundance of zooplankton collected with the 200 µm net was between two and 20 times lower than samples taken with the 45 µm net. The most pronounced differences were observed for the adults and copepodids of the small genera Oithona, Oncaea and Microsetella. Thus, to manage and understand the transfer of primary production up the food chain in the Aegean Sea, the smaller fraction of copepods should be taken into account in future investigations.