Ammonit aus der Jurazeit - Epipeltoceras berrense
Epipeltoceras berrense (FAVRE). Oxfordium, untere Bimammatum-Zone, semiarmatum-Subzone, laufenensis-Bank, 11 m über Fucoidengrenzbank, glaukonitische Fazies. Gewand Rübenhau, Nordseite der Lochen bei Balingen, Zollernalbkreis 1978.
Information
| Section | Natur: Fossilien & Präparate |
| Folders | Minerale•Fossilien |
| Views | 1,532 |
| Published | |
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| License |
Exif
| Camera | SZ-17 |
| Lens | --- |
| Aperture | 4.4 |
| Exposure time | 1/100 |
| Focus length | 11.9 mm |
| ISO | 160 |
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