Iron sulfides and magnitite were also found. These minerals are commonly produced by anaerobic bacteria and other microscopic organisms.
A)
Low maginfication of Fe-rich rim containing fine grained magnetite and
Fe-sulfide phases and their association with the surrounding carbonate.
B) High magnication
of a magnetite-rich area in A) showing the distribution of individual magnetite
crystals. C) high magnification of a pyrrhotite-rich region showing the
distribution of individual pyrrhotite particles (two black arrows in the
centre) together with magnetite (other arrows) within fine-grained carbonate.
Courtsey of Science on Line.