Abstract
Accepting presence of sulfate (SO_4~(2-)) in francolite lattice as an isomorphous substitution for phosphate (PO_4~(3-)), Nathan and Nielsen and Benmore et al. investigated sulfur isotopes of the sulfate within francolite for the marine phosphorites formed since the Permian, and origin, sedimentary and diagenetic environments of phosphorites. Here, we
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