“…Mercury enters the sea by river transport and following wet and dry deposition from the atmosphere. In surface water, it is subjected to light-dependent biotic and abiotic redox processes that transform ionic mercury to volatile Hg 0 (Amyot et al, 1994;Costa and Liss, 2000;Kim and Fitzgerald, 1986;Kuss et al, 2015;Mason et al, 1995), which is subjected to evasion from the sea surface. Mercury emission by the ocean accounts for about one-third of the mercury in the atmosphere (Pirrone et al, 2013;Selin et al, 2008).…”