The response of phytoplanktonic biomass to the changes in the physical and chemical structure produced by an upwelling event is analyzed in a daily scale. The results show a physical-chemical coupling, and a high spatial and temporal variability in the cholorophyll concentration. The response of chlorophyll was characterized by a two or three days lag to favorable conditions, and a change in the phytoplanktonic fractions responsible of the most important concentration was observed. The study period coincided with "El Nino" 1997-1998 presence, but the results do not show anomaly conditions associated with this event.
CITATION STYLE
Santander, E., Herrera, L., & Pizarro, J. (2001). Fluctuación diaria del fitoplancton en la capa superficial del océano durante la primavera de 1997 en el norte de Chile (20°18′S): I. Biomasa Pigmentaria. Revista de Biologia Marina y Oceanografia, 36(2), 141–153. https://doi.org/10.4067/s0718-19572001000200003
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