Ammonit aus der Jurazeit - Perisphinctes colubrinus
Perisphinctes colubrinus (REINECKE). Oxfordium, höhere Bimammatum-Zone, oberer Teil des stärker glaukonitischen Abschnitts, ca. 19 m über Fucoidengrenzbank. Gewand Rübenhau, Nordseite der Lochen bei Balingen, Zollernalbkreis 1978.
Information
| Section | Natur: Fossilien & Präparate |
| Folders | Minerale•Fossilien |
| Views | 1,568 |
| Published | |
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Exif
| Camera | SZ-17 |
| Lens | --- |
| Aperture | 3.6 |
| Exposure time | 1/60 |
| Focus length | 6.6 mm |
| ISO | 100 |
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