Ammonit aus der Jurazeit - Perisphinctes sp.
Perisphinctes sp. Oxfordium, höhere Bimammatum-Zone, oberer Teil des stärker glaukonitischen Abschnitts, ca. 16 m über Fucoidengrenzbank. Gewand Rübenhau, Nordseite der Lochen bei Balingen, Zollernalbkreis 1977.
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| Section | Natur: Fossilien & Präparate |
| Folders | Minerale•Fossilien |
| Views | 1,289 |
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