Mass accumulation of mucilage caused by dinoflagellate polysaccharide exudates in Tasman Bay, New Zealand

At about 20-year intervals, since at least the 1860s, there have been accounts of the accumulation of large quantities of mucilage in the waters off the northern coast of the South Island of New Zealand. On a few occasions these events have been associated with harmful effects, such as the mass mortality of marine fauna and the impediment of fishing activities, though previous attempts to identify the causative organism(s) or the environmental conditions which promote its development have been unsuccessful. In January 2000, there was a moderate re-occurrence of mucilage accumulation in Tasman Bay that led to the identification of the primary origin of this material as the planktonic, thecate, dinoflagellate Gonyaulax hyalina (Ostenfeld et Schmidt). Macro-aggregate accumulation was occurring in the water column when dinoflagellate cell numbers were relatively low. Experimental work on cultures of this organism showed that the dinoflagellate produced transparent exo-polymers (TEPs) composed primarily of galactose and glucose monomers (44.8 and 29.6 mol%, respectively). Analysis of natural and cultured mucilage showed this had a high inorganic content (>60% (w/w)). A substantial proportion (40% (w/w)) of this inorganic fraction was composed of calcium that apparently played an important role in stabilizing the gel. Phosphorus was also enriched in the mucilage. It is hypothesized that the high inorganic N/P ratio observed in the water column at the time of mucilage formation was an effect rather than a cause of this event, which resulted in the scavenging of particulate material from the water column and enrichment of sediments and bottom waters with organic material and phosphorus.