Large quantities of carbonate mud are found in suspension, with concen
trations reaching 80 mg l(-1), in the lagoon of Mataiva Atoll, French
Polynesia. Residence time of water in the lagoon is about 73 days. Car
bonate particles are exported offshore in a negatively buoyant plume t
hat sinks in oceanic waters. The carbonate particles are from resuspen
sion of abraded carbonate of biological origin. The negative buoyancy
is induced by evaporative cooling of turbid lagoon water, turbidity re
sulting from wave-driven suspension of calcareous sediment. Contaminat
ed mine water should be released at depth, offshore, as a negatively b
uoyant plume to sink in oceanic waters.