Abstract
The effect of seasonal temperature change on the release of methylated arsenic from macroalgae, phytoplankton and sediment porewaters has been investigated by a series of controlled laboratory experiments. The appearance of dissolved arsenic species in the overlying waters was monitored using a coupled hydride generation/GC AA analytical technique. The liberation of dissolved arsenic species by the macroalgae Ascophyllum nodosum was examined under estuarine conditions at 5 Β°C and 15 Β°C. At the lower temperature the release rates were 0.2 ΞΌg kg^β1^ h^β1^ (wet weight of material) for monomethylarsenic (MMA) and 0.5 ΞΌg kg^β1^ h^β1^ for dimethylarsenic (DMA), whereas at 15 Β°C the rates were 0.4 ΞΌg kg^β1^ h^β1^ and 3.2 ΞΌg kg^β1^h^β1^, respectively. Incubation experiments were also carried out at 15 Β°C using the diatom Skeletonema costatum. During the log growth phase, when chlorophyll a concentrations were in the range 1β5 ΞΌg dm^β3^, the rate of appearance of DMA in the water was βΌ3 ng dm^β3^ h^β1^. Sediment samples from the freshwater and seawater endβmembers of the Tamar Estuary, UK, were incubated under natural conditions at 5 Β°C and 15 Β°C. The freshwater sediments released DMA in preference to MMA; the concentrations of both species increased exponentially and reached a steady state in the overlying water after 250 h. Considerably more DMA was produced at 15 Β°C than at 5 Β°C, whilst the amount of MMA produced appeared to be insensitive to the temperature increase. In contrast, the seawater sediments always produced more MMA than DMA and the increase in temperature had little effect on the production of either MMA or DMA.
The results of the laboratory experiments were compared with field observations in temperate estuaries, including the Tamar Estuary. The implications of changes of water temperature on the fate of arsenic in estuaries is discussed and modifications to the estuarine arsenic cycle are proposed.