HPLC analysis of chlorophyll a breakdown products to interpret microalgae dynamics in a shallow bay

Phytoplankton production is determined by growth, senescence, sinking and zooplankton grazing. In an attempt to follow algal senescence and grazing, some authors have used HPLC fluorescence detection of chlorophyll a breakdown products. Laboratory grazing experiments have shown that copepods reduce chlorophyll a from diatoms leading to an increase in pheophytin a rather than pheophorbide a. However, field measurements only indicated a slight increase of pheopigment concentrations in summer. During this period, high heterotrophic activities (zooplankton and bacteria) seemed to be responsible for rapid pheopigment disappearance. On the other hand, highest chlorophyllide a levels appeared to be related to spring accumulation of nutrient-limited senescent algae. While increases in pheophytin a accounted for chlorophyll a consumption, changes in pheophorbide a concentrations could be linked to chlorophyllide a abundance. These results suggest that laboratory studies cannot be uncritically extrapolated to the field.