Fig. 3From: New coelacanth material from the Middle Triassic of eastern Switzerland, and comments on the taxic diversity of actinistans Ticinepomis peyeri, holotype (PIMUZ T 3925), Monte San Giorgio, upper part of the Besano Formation (Grenzbitumenzone), Middle Triassic (Early Ladinian) of Canton Ticino. a Part. b Counterpart. Scale bars 10 mmBack to article page