Hong Kong’s worst “red tide”—causative factors reflected in a phytoplankton study at Port Shelter station in 1998

Abstract

From March through April 1998, a massive “red tide” occurred in coastal waters of south China, including Hong Kong. The “red tide” rapidly killed various species of caged fish and affected coral fishes, killing a few of them, and caused great economic loss and ecological damage. Samples collected from a permanent station located in Port Shelter revealed a new dinoflagellate species, Karenia digitata which was suspected to be the causative species of this “red tide”. Species composition and abundance analysis revealed that an algal bloom persisted in Port Shelter during this entire period. Diatoms and dinoflagellates were the two main groups which dominated the phytoplankton and, in general, when there was an increase in the density of diatoms there was a decline in the density of dinoflagellates, and vice versa. The suspected “red tide” causative species together with other dinoflagellate species started to bloom in late February and reached their highest density on 18 March, when fish kills were first reported at Crooked Island, a semi-enclosed bay to the northeast of Hong Kong. During a 16-week period, dinoflagellate species dominated three times, and coincided with low wind speeds. Constant salinity and a continuing increase in sea surface water temperature suggested warm water intrusion into Hong Kong’s coastal waters during this “red tide” bloom period. Various nutrient elements, e.g. NH 4-N, total Kjeldahl nitrogen (TKN), and PO 4-P were high at the beginning of the bloom but experienced a sharp decrease thereafter. It is suggested that this early 1998 massive “red tide” in Hong Kong waters might have been triggered by a synchronous appearance of optimal climatic, nutritional and hydrographic conditions.