“…Inertinite in general, and fusinite in particular, have been treated as important indicators of "dry" conditions within mires in some petrographically based reconstructions of environments (Hacquebard and Donaldson, 1969;Gelification Index of Diessel, 1982Harvey and Dillon, 1985;Grady and Eble, 1990;Eble and Grady, 1990;Lamberson et al, 1991;Kalkreuth et al, 1991 but not by Calder et al, 1991or Calder, 1993. For fusinite, this inference appears to be based on the assumption that burning is likely to be more frequent in parts of mires with exposed, even if wet, substrates.…”