Versteinerte Seeigelstachel aus der Jurazeit
Seeigelfauna. Oxfordium, untere Bimammatum-Zone, semiarmatum-Subzone, ca. 3 m über Fucoidengrenzbank. Gewand Rübenhau, Nordseite der Lochen bei Balingen, Zollernalbkreis 1977.
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| Section | Natur: Fossilien & Präparate |
| Folders | Minerale•Fossilien |
| Views | 1,897 |
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alicefairy 07/11/2022 8:20
sehen hübsch ausLg Alice