Deep chlorophyll a maxima in the Red Sea observed by in-vivo flash fluorometry

An investigation of the hydrography and the population, production and biomass of plankton in the Red Sea, carried out during the METEOR cruise in summer 1987, aimed to describe the ecosystem characteristics during the SW monsoon period. Vertical profiles of in-vivo chlorophyll fluorescence intensity, measured in the presence of chlorphenyl-dimethyl-urea (CMU), are presented. Variations in the fluorescence pattern were observed and assumed to be due to the influence of a reef and surface influx of nutrient rich water from the Gulf of Aden into the Red Sea. This northward influx was driven by SE winds, caused by an unusual northward shift of the innertropical convergence zone up to 20°N in summer 1987. Integrated chlorophyll a values were calculated from fluorescence data. They showed a slight increase from north to south and higher pigment contents in August (8.7–20.2 mg m^–2) than in July (3.3–9.0 mg m^–2), the latter was attributed to the above mentioned influx. Calibration of the fluorescence measurements using cultures of a green alga and cyanobacterium indicated that there may have been an underestimate of the contribution of Oscillatoria populations to the chlorophyll a concentration of the samples. Fluorescence peaks were recorded in the lower part of the euphotic zone, indicating a deep maximum of phytoplankton and/or an increase in chlorophyll fluorescence per unit biomass at these depths.