“…Hitherto, the crystallisation of aragonite otoliths was not thought to have evolved until the separation of teleosts from other Actinoperygian fishes ( e.g ., sturgeon, paddlefish, gar; Carlström ; Fermin et al ., ; Gauldie, , Pracheil et al ., in press). Although small calcite and aragonite inclusions have indeed been observed in the otoliths of other acipenserids, they were believed to be an artifact of preservation or a transformation to more stable crystalline forms post‐dissection rather than true observations of non‐vaterite otoliths (Carlström, ; Lychakov, ; Schulz‐Mirback et al ., ). Mechanical and thermodynamic testing of vaterite transformation confirmed, however, that although the vaterite polymorph found in Lake Sturgeon otoliths is metastable, it is indeed resistant to transformation to more stable polymorphs under routine methods (Pracheil et al ., ).…”