The mineral formerly described as fougèrite has been found to be an intimate intergrowth of two phases with distinct
Fe2+:Fe3+ ratios. The phase with
Fe2+:Fe3+ = 2:1 retains the name fougèrite; that with
Fe2+:Fe3+ = 1:2 is defined as the new species
trébeurdenite. Both belong to the
Fougèrite Group (Mills et al., 2012).
Fougèrite is unstable in air at normal conditions (Trolard et al., 2007); the green (or green-black, blackish), hexagonal, transparent platelets transform quickly into yellow-brown to brown, opaque, often poorly crystalline, brittle iron oxyhydroxides (
limonite,
goethite,
lepidocrocite). Known previously as "Green Rust", mainly from iron-rich slags.
Varieties containing Zn retain their green colour and transparency (Blaß et al., 1997).
The characteristic blue-green colour (5BG6/1 in the Munsell system) of fougèrite has long been used as a universal criterion in soil classification to identify Gleysols (Trolard et al., 2007).
One of six minerals proposed to be essential for life emergence. Actually, one of two "vital" candidates due to "comprising precipitate membrane", the other one being
mackinawite (Russell & Pone, 2020).