Ability of marine eukaryotic red tide microalgae to utilize insoluble iron

Abstract

Iron is an essential trace metal and a limiting factor for microalgal growth, but bioavailable dissolved iron concentrations in seawater are low. Microalgal blooms have frequently occurred in coastal areas under such iron limitation accompanied by mass mortalities of fish and bivalves. Their massive growth despite physiological iron-deficiency has long been an enigma, because most of them cannot grow in chemically defined artificial media. We developed a feasible artificial medium for the culture of many species of red tide microalgae modified for investigation of iron utilization. Here, we report on the ability of marine eukaryotic red tide microalgae to utilize insoluble iron. Some microalgal species could utilize particulate FePO 4 and FeS for growth. Particulate FePO 4 was available for the growth of the raphidophyte Heterosigma akashiwo, the dinoflagellate Heterocapsa triquetra and the diatom Ditylum brightwellii. The dinoflagellates Heterocapsa circularisquama and Karenia mikimotoi, and the cryptophyte Rhodomonas ovalis utilized both particulate FePO 4 and particulate FeS for growth. In contrast, particulate FeO(OH) and Fe 2O 3 did not support the growth of any of the red tide microalgae examined. Except for Chattonella species (Raphidophyceae), the growth of red tide microalgae were confirmed in the medium with very easily soluble FeCl 3 added. The order of bioavailability of tested iron-source species were Fe–EDTA > FeCl 3 > FePO 4 > FeS > FeO(OH), Fe 2O 3 for most of microalgae examined, although for H. circularisquama the utilization of FeCl 3 was higher than that of Fe–EDTA. The results suggest that red tide microalgae show different patterns of specific strategies for the utilization of various iron sources. The occurrence of red tides in coastal areas may depend on the combination of microalgal species and insoluble iron species present.