The biotransformation of Hg(II) by cyanobacteria was investigated under aerobic and pH-controlled culture conditions. Mercury was supplied as HgCl 2 in amounts emulating those found under heavily impacted environmental conditions where bioremediation would be appropriate. The analytical procedures used to measure mercury within the culture solution, including that in the cyanobacterial cells, used reduction under both acid and alkaline conditions in the presence of SnCl 2 . Acid reduction detected free Hg(II) ions and its complexes, whereas alkaline reduction revealed that meta-cinnabar (-HgS) constituted the major biotransformed and cellularly associated mercury pool. This was true for all investigated species of cyanobacteria: Limnothrix planctonica (Lemm.), Synechococcus leopoldiensis (Racib.) Komarek, and Phormidium limnetica (Lemm.). From the outset of mercury exposure, there was rapid synthesis of -HgS and Hg(0); however, the production rate for the latter decreased quickly. Inhibitory studies using dimethylfumarate and iodoacetamide to modify intra-and extracellular thiols, respectively, revealed that the former thiol pool was required for the conversion of Hg(II) into -HgS. In addition, increasing the temperature enhanced the amount of -HgS produced, with a concomitant decrease in Hg(0) volatilization. These findings suggest that in the environment, cyanobacteria at the air-water interface could act to convert substantial amounts of Hg(II) into -HgS. Furthermore, the efficiency of conversion into -HgS by cyanobacteria may lead to the development of applications in the bioremediation of mercury.Mercury in the form of divalent ions constitutes the bulk of that in soils, where it is bound to organic compounds, to clay, and as sulfides (31). Although industrialization in the beginning of the last century is the cause of most of the mercury contamination found in the environment today, rainfall continues to carry mercury [Hg(II)] into aquatic and terrestrial systems worldwide (16,44). Despite a comprehensive knowledge of the mercury cycle and the aquatic chemistry of its constituents (12, 43, 52), several microbial taxa have not been characterized with respect to their roles in the biotransformation of this heavy metal.Several mercury biotransformation mechanisms have been described previously (4,12,39,41), and of these, prokaryotic methylation and reduction to Hg(0) may play only limited roles in the biotransformation of Hg(II) in aquatic environments (15,19). Furthermore, the reduction reaction simply refracts meteorologically precipitated Hg(II) back into the atmosphere. As such, it follows that other processes must make significant contributions to the biogeochemical cycle of Hg even though relative quantitative data are scarce (31). Insight into this area requires an understanding of the major biotransformation processes leading to mercury retention in ecosystems.The lack of quantitative, mechanistic data behind cellular accumulation versus that for volatilization of Hg is evident even in the eukar...