“…This is largely due to the extremely low solubility of the thermodynamically stable Fe(III) oxidation state at circumneutral pH in well-oxygenated soils and surface waters. However, in many coastal floodplains formed during the Holocene period, massive quantities of Fe (and Al) are periodically discharged from disturbed acid sulfate soils to surrounding estuarine and coastal environments (Green et al, 2006a(Green et al, , 2006bMacdonald et al, 2007). The large-scale deoxygenation and acidification of these aquatic environments, caused in part by the oxidation of Fe(II) and subsequent hydrolysis of Fe(III), often results in the mass mortality of gilled organisms and is of particular concern in the tropical and sub-tropical regions of south east Asia and north east Australia (Dent and Pons, 1995;White et al, 1997).…”