Ammonit aus der Jurazeit - Epipeltoceras bimammatum
Epipeltoceras bimammatum (QUENSTEDT). Oxfordium, höhere Bimammatum-Zone, ca. 20 m über Fucoidengrenzbank, Haldenfund, glaukonitische Fazies. Gewand Rübenhau, Nordseite der Lochen bei Balingen, Zollernalbkreis 1979.
Information
| Section | Natur: Fossilien & Präparate |
| Folders | Minerale•Fossilien |
| Views | 1,379 |
| Published | |
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| License |
Exif
| Camera | SZ-17 |
| Lens | --- |
| Aperture | 4.4 |
| Exposure time | 1/100 |
| Focus length | 11.9 mm |
| ISO | 250 |
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