Ammonit aus der Jurazeit - Perisphinctes (Dichotomoceras) bifurcatus
Perisphinctes (Dichotomoceras) bifurcatus (QUENSTEDT). Oxfordium, höhere Bimammatum-Zone, oberer Teil des stärker glaukonitischen Abschnitts, ca. 16 m über Fucoidengrenzbank. Gewand Rübenhau, Nordseite der Lochen bei Balingen, Zollernalbkreis 1977.
Information
| Section | Natur: Fossilien & Präparate |
| Folders | Minerale•Fossilien |
| Views | 1,303 |
| Published | |
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| License |
Exif
| Camera | SZ-17 |
| Lens | --- |
| Aperture | 4 |
| Exposure time | 1/80 |
| Focus length | 8.9 mm |
| ISO | 125 |
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