“…The resulting acidic solution, containing metals (Fe, Mn, Zn, Cu ... ) and reduced sulfur compounds such as sulfides and HzS, percolates up to the sea floor where it mixes with the cold surrounding ocean water (4°C), forming mineral deposits and different types of vents (Tunnicliffe et al, 1998;Zierenberg et al, 2000). These chemicals provide a source of energy and nutrients to chemoautotrophic and other organisms present in this environment (Felbeck, 1981;Felbeck et al, 1981;Cavanaugh et al, 1981;Gaill, 1993;Fisher, 1996;Minic and Herve, 2004;Minie et al, 2006). Organisms include a large variety of microorganisms (Eubacteria, Archaea, mainly extremophiles) and more than five hundred animal species from twelve different phyla (Desbruyeres et al, 2006).…”