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Collection: Stramberg, Moravia Štramberk, Nový Jičín District, Moravian-Silesian Region, Czech Republic
| Age | 152.1 - 145 Ma (Late Jurassic) |
|---|---|
| Interval | Tithonian |
| Lat/Long | 49.59,18.12 |
| Co-ordinates derived from | based on nearby landmark |
| Location | Stramberg |
| Mindat.org Region (for given coordinates) | Štramberk, Nový Jičín District, Moravian-Silesian Region, Czech Republic |
| Geographic Scale | outcrop |
| Formation | Stramberger |
| Stratigraphic Scale | group of beds |
| Lithology | "limestone" |
| Environment | carbonate indet. |
Associated Collections
| Collection | Formation | Member | Lithology | Age |
|---|---|---|---|---|
| Stramberg (Mähren) (Wien collection) | Stramberger | "limestone" | 152.1 - 145 Ma (Late Jurassic) |
Recorded Fossils
| Accepted Name | Hierarchy | Preservation | Age |
|---|---|---|---|
 Paracymatoceras asperspecies | Animalia : Mollusca : Cephalopoda : Nautilida : Nautilidae : Paracymatoceras : Paracymatoceras asper | aragonite body | 152.1 - 145 Ma Late Jurassic |
| Pseudonautilus geinitzi species | Animalia : Mollusca : Cephalopoda : Nautilida : Pseudonautilidae : Pseudonautilus : Pseudonautilus geinitzi | aragonite body | 152.1 - 145 Ma Late Jurassic |
| Pseudaganides stromeri species | Animalia : Mollusca : Cephalopoda : Nautilida : Pseudonautilidae : Pseudaganides : Pseudaganides stromeri | aragonite body | 152.1 - 145 Ma Late Jurassic |
| Aulaconautilus picteti species | Animalia : Mollusca : Cephalopoda : Nautilida : Pseudonautilidae : Aulaconautilus : Aulaconautilus picteti | aragonite body | 152.1 - 145 Ma Late Jurassic |
| Pseudaganides klebelsbergi species | Animalia : Mollusca : Cephalopoda : Nautilida : Pseudonautilidae : Pseudaganides : Pseudaganides klebelsbergi | aragonite body | 152.1 - 145 Ma Late Jurassic |
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
