“…The Fe(II) that remains in solid forms is not well characterized (153,323) and may be in the form of various Fe(II) minerals such as vivianite (30,71,95,131,265), siderite (30, LOVLEY 129, 265, 326), hydroxides (323), mixed Fe(II)-Fe(III) compounds (182,193,261,264,323), and Fe(II) silicates (30, 122, 261) as well as amorphous Fe(II) adsorbed onto various solid phases, including clays and organic matter (134,306,323). Iron sulfides can be important sinks of Fe(II) in marine environments and may also be important in freshwater environments such as swamps, which are unusually rich in organic compounds and have substantial releases of sulfur from organic matter (29).…”