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The marine Cyanobacteria Synechococcus and Prochlorococcus contribute amongst 32 and 80 of the total principal productivity in oligotrophic oceans (Goericke and Welschmeyer, 1993; Li, 1995; Liu et al., 1997; Veldhuis et al., 1997; Rocap et al., 2002) and about 50 on the fixed carbon in some oceanic regions (Zwirglmaier et al., 2007). Also, the Marine Cluster-A group (MC-A or Synechococcus subcluster five.1) is believed to become the dominant Synechococcus group within the euphotic zone of open ocean and coastal waters (Fuller et al., 2003). Synechococcus WH8102 can be a well-studied Sargasso Sea isolate from the MCA group with an accessible genome sequence (Waterbury et al., 1986; Scanlan, 2003; Palenik et al., 2003). Preceding culture research examining the influences of metals on this organism showed that at low zinc (Zn) concentrations increased cadmium (Cd) concentrations inhibited development, whereas this was not observed at larger Zn concentrations (Saito et al., 2003). Cd and Zn have nutrient-like distributions inside the ocean, meaning they may be depleted in surface waters and enhance with depth,implying that Cd and Zn are taken up by microorganisms within the surface water and remineralized at depth (Boyle et al., 1976; Bruland, 1980). Dissolved total Zn may possibly reach concentrations up to 9 nM at depth, whereas Cd could reach up to 1 nM (Bruland, 1980, 1992). Notably, this excess of dissolved Zn over Cd is common of deepwater ocean environments, on the other hand, this difference can lower in surface waters as Zn is depleted (Sunda and Huntsman, 2000; Saito et al., 2010). Zn is vital towards the proper functionality of lots of enzymes and is thought to be an important metal in living organism.