“…Lack of phosphorus in the mantle matter and in the mandibles reveals that the preservation of the non-biomineralized soft tissue was not controlled by a phosphorus-rich medium. Contrary to the mantle and mandibles, the shell wall in Austrotrachyceras is calcareous; it is composed of O (65-80 %), C (25 %), Ca (8-16 %), Sb (2 %), Mo (2 %), Mg, K (each 1 %), and S, Si, Mn, Fe (each < 1 %) (Doguzhaeva et al , 2007b. The low oxygen depositional environment (Griffith 1977) responsible for carbonization of the mantle and the mandibles of Austrotrachyceras also favored the preservation of the muscular mantle, ink sacs and arm-hooks of the coleoid Phragmoteuthis bisinuata (Doguzhaeva et al 2007b, Doguzhaeva andSummesberger 2012).…”