A COMPARISON OF MARINE PLANKTONIC AND SEDIMENT CORE DIATOMS IN HONG-KONG WITH EMPHASIS ON PSEUDO-NITZSCHIA

Potentially toxic diatoms belonging to the genus Pseudo-nitzschia were observed for the first time in plankton samples from Hong Kong collec ted in 1996. To determine whether potentially toxic diatoms had become more common during the last six decades, three gravity cores were tak en from the anaerobic sediments of Kowloon Bay in Victoria Harbour. An aerobic sediments are thought to be ideal for palaeoecological reconst ructions because their vertical stratigraphy is undisturbed by bioturb idation. Analysis of the Kowloon Bay sediment cores indicated that ver y few individual diatoms belonged to the genus Pseudo-nitzschia, even though Pseudo-nitzschia was found in abundance in many of the plankton samples taken from a nearby site. The relative absence of Pseudo-nitz schia frustules was interpreted as indicating that these thin walled, poorly silicified, planktonic diatoms failed to preserve in the saline (32-34 parts per thousand), slightly alkaline (pH 7.6-7.8), anaerobic sediments of Kowloon Bay. Dissolution of thinly silicified diatoms ra ther than predation was believed to be the reason for their virtual ab sence in the core. The anaerobic conditions near the bottom of Kowloon Bay and the shallowness of the Bay, 12 m, makes predation an unlikely explanation. Diatom abundance declined in the sediment cores below a depth of 15 cm (ca 1955). This was attributed to the decrease in nutri ent loading to Victoria Harbour prior to 1955 rather than enhanced dia tom dissolution in the deeper sediments. Benthic diatoms became propor tionately more abundant below the 15 cm core depth.