Ammonit aus der Jurazeit - Perisphinctes (Dichotomoceras) bifurcatus
Perisphinctes (Dichotomoceras) bifurcatus (QUENSTEDT). Oxfordium, untere Bimammatum-Zone, semi-armatum-Subzone, laufenensis-Bank, 11 m über Fucoidengrenzbank, glaukonitische Fazies. Gewand Rübenhau, Nordseite der Lochen bei Balingen, Zollernalbkreis 1978.
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| Section | Natur: Fossilien & Präparate |
| Folders | Minerale•Fossilien |
| Views | 1,602 |
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