File:Pycnodonte vesiculare left valve.jpg

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Deutsch: Eine linke, stark konvexe Klappe der spätkreidezeitlichen gryphaeiden Muschel Pycnodonte (Phygraea) vesiculare, schräg von vorne gesehen. Die Schale ist von Bryozoen bewachsen. Das Stück entstammt den mürben Hochsee-Kalksteinen („Schreibkreide“) des Unter-Maastricht (Rügen-Member der Hemmoor-Formation) der Region um Sassnitz im Nordosten der Insel Rügen.
English: A left, strongly convex valve of the Late Cretaceous gryphaeid bivalve Pycnodonte (Phygraea) vesiculare in oblique anterior view. The shell is overgrown by bryozoans. The specimen was collected from the soft Lower Maastrichtian hemipelagic limestones (Rügen Member of Hemmoor Formation) of the Sassnitz area, Rügen Island, NE Germany.
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Author Gretarsson
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Internal views of both valves of the same individual

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current16:27, 10 August 2017Thumbnail for version as of 16:27, 10 August 20171,042 × 1,158 (731 KB)Gretarsson (talk | contribs){{Information |Description ={{de|1=Die linke, stark konvexe Klappe der spätkreidezeitlichen gryphaeiden Muschel ''Pycnodonte (Phygraea) vesiculare'', schräg von vorne gesehen. Die Schale ist von Bryozoen bewachsen. Das Stück entstammt den mürben...

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