Biogeochemistry and effects of copper,manganese and zinc added to enclosures in Island Billabong,Magela Creek,northern Australia

Three large plastic enclosures (5 m diam, volume 40 m³) were used to study the effects of copper, manganese and zinc, on the phytoplankton community in Island billabong, a floodplain billabong (waterhole) situated in the Magela Creek in tropical northern Australia. Copper was added to one enclosure, and manganese and zinc to another, to give initial concentrations around ten times the normal wet season values. The enclosures and the billabong were monitored over a ten week period towards the end of the dry season, with the enclosures allowed to stabilise for four weeks before the metals were added.The control enclosure adequately simulated the temperature and pH changes in the billabong. The trends in conductivity, dissolved oxygen and major ion concentrations were similar in the enclosure and the billabong, with the minor differences observed attributed to either epiphytic growth on the enclosure walls (influenced dissolved oxygen, pH and bicarbonate concentration) or ingress of sulphate-rich groundwater into the billabong (influenced sulphate concentration and conductivity). Major differences in both the composition of species and the size of the phytoplankton populations were observed between the three enclosures and between the control enclosure and the billabong. This variability reflects the great natural variability in the phytoplankton communities in tropical lentic systems, and means that enclosures are unlikely to adequately simulate the biological communities in the billabongs.The control enclosure appeared to simulate quite well the longer term changes in total concentration and speciation of the three metals (copper, manganese & zinc) in the billabong. The mean concentrations of copper and zinc were similar in the two systems, although the mean concentration of manganese in the billabong was almost double that in the enclosure, possibly due to ingress of manganese-enriched groundwater. Particulate forms dominated the speciation of copper and manganese. There was considerable short term variation in both total metal concentration and speciation in both the enclosure and the billabong. This variability appears to be a feature of these small tropical waterbodies.The added heavy metals were found to have minimal detrimental effect on the phytoplankton community in each metal-loaded enclosure. The high natural variability in the phytoplankton community in these tropical systems will make it difficult to separate natural changes from those caused by low level contamination from mining operations should this occur.All three metals were rapidly removed from the water column, so that by the end of the six week period, only ca. 5% of each added metal remained in the water column. Association with the particulate matter (phytoplankton, abiotic particulate matter and MnO_x in enclosure 2) followed by sedimentation was the major removal pathway. Epiphytes growing on the enclosure walls appeared to have a minor influence (<10% of the total amount of metal added) on the removal of the added metals. For copper, uptake by phytoplankton followed by sedimentation was the major (65%) removal process. Manganese and zinc, added together, were found to influence each other. The major manganese removal process (60%) was rapid (ca. 3 days) involving bacterial oxidation and sedimentation of the MnO_x formed. This material appeared to have little influence on the behaviour of zinc, possibly because other particulate matter competed more effectively for the zinc. A further 30% of the added manganese was removed via initial adsorption to other particulate matter, possibly phytoplankton. Approximately one third of this adsorbed manganese (10% of the total added) appeared to undergo delayed oxidation some 8 days after the initial additions, and the heavier particles settled out more rapidly. This path was responsible for removing the major amount (ca. 60%) of the added zinc. We hypothesis that the sorbed zinc inhibited the bacterial oxidation of the manganese. A further 25% of the zinc was removed in association with a burst of phytoplankton activity. The occurrence of bursts in the phytoplankton activity, when populations can increase very substantially and then decrease again, all within the space of a day, appears to be an important mechanism for removing copper and zinc from the water column in these tropical water bodies