The extracellular polysaccharide production by marine diatoms is a significant route by which photosynthetically produced organic carbon enters the trophic web and may influence the physical environment in the sea as observed for example when massive aggregation events on basin scale occur. Many papers showed that the aldose signatures of marine DOM obtained from different
seawater samples around the world is similar to that determined on cultured phytoplankton DOM and that the carbohydrate production could be very different among the species selected, growth and environmental conditions. These results are very important in order to understand the role of algal exudation in the aggregation processes observed in all of the seas and in general in carbon cycling in the euphotic zone. Many authors showed that cultured diatoms growth in P-limiting condition determines an increase of polysaccharides
exudated by different diatoms species both pelagic and benthic.
