Volcanic glass is probably chemically the most reactive material that is deposited in the oceans, as aerosol, as suspended river load from volcanic terrain, or as part of the extrusive layer of the oceanic crust. The total volume of this material is large, probably on the order of about 10~6g/a, providing the potential of very large chemical fluxes. Recent studies have shown that microbial activity plays an important role in the dissolution of glass in the marine environment, through mediation of the dissolution process, and, presumably, utilization of components of the glass freed up during this process (e.g. Thorseth et al., 1995; Fumes et al., 1996, Giovarmoni et al., 1996; Staudigel et al., 1995). The interaction between biota and volcanic glass is likely an influence on local ecology as well as on the chemical mass balance between biosphere, hydrosphere and lithosphere. We carried out a series of experiments to explore further the role of colonizing microorganisms on the dissolution of glass. All experiments were done with natural populations of microbes from surface sea water at two temperatures, under the ambient light intensity in the laboratory and in the dark. Open system experiments were done with a constant supply of fresh seawater. The closed system apparatus included 501 seawater reservoirs and a FEP Teflon column setup with approximately 150 g of glass (Staudigel et al., 1997). A closed system with autoclaved components and seawater served as an abiotic control. More recent continuous flow experiments include approximately 300 g of glass and a continuous flow of 20 1 of fresh sand-filtered seawater per day. We carried out an experiment at 60 ~ C and compared this to an experiment at 16~ Run products were analysed for major and trace elements and for changes in glass surface structure and in microbial colonization by SEM. Microbial populations were characterized with a variety of metabolic tests. Closed-system sterile control experiments remained sterile for periods exceeding 450 days showing that these experimental conditions do not allow for microbial contamination. Biologically active experiments display a diverse population of microbes, including a series of algae including Si utilizers (diatoms) and algae with aragonitic exosceletons (halimeda). In cold experiments we identified several chemolithotrophs including a rod-shaped motile sulphur-oxidizer, probably Thiobacillus sp., and two strains of rod-shaped non-motile ammoniaoxidizers. Photoautotrophs, all cyanobacteria, include Spirulina, Phormidium, Anacystis, and a sheathed, filamentous strain that is probably either Anabaena or Nostoc. 60~ experiments displayed no significant thermophile activity for the first two months of its duration. However, after about g months we could identify a diverse population of thermophilic microorganisms, including heterotrophs, sulphuroxidizers, nitrite-oxidizers and ammonia-oxidizers. These results suggest that surface seawater has the means to transport thermophilic microbial life, even though in our experiments it took between two to eight months for them to appear. Overall these results suggests that surface seawater contains a sufficiently diverse environmental microbial population that can adjust to a wide range of conditions, and newly developed hydrothermal systems do not remain abiotic for a long time after initiation. Such processes are expected to occur not only in the mixing zone of
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