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Kossen - Hochalm, Unit 2, Austria
| Formation | Kossen |
|---|---|
| Member | Hochalm, Unit 2 |
| Age: | 209 - 201 Ma Mesozoic |
| Interval | Rhaetian |
| Lithology | carbonate, "limestone", "carbonate"/marl |
| Number of Collections | 9 |
| Number of Occurrences | 40 |
Recorded Sample Locations
| Location | Region | Stratigraphic Name |
|---|---|---|
| Neuhaus 21 | Gaming, Scheibbs District, Lower Austria, Austria | Kossen - Hochalm, Unit 2 |
| Hochalm B5 | Unken, Zell am See District, Salzburg, Austria | Kossen - Hochalm, Unit 2 |
| Neuhaus A40 | Gaming, Scheibbs District, Lower Austria, Austria | Kossen - Hochalm, Unit 2 |
| Kossen B1 | Kössen, Kitzbühel District, Tyrol, Austria | Kossen - Hochalm, Unit 2 |
| Hochalm B10 | Unken, Zell am See District, Salzburg, Austria | Kossen - Hochalm, Unit 2 |
Associated Units
| Stratigraphic Name | Age | Lithology | Occurrence Records |
|---|---|---|---|
| Kossen - 2 | 209 - 201 Ma Mesozoic | siliciclastic | 9 |
| Kossen - 3 | 209 - 201 Ma Mesozoic | siliciclastic, "carbonate" | 45 |
| Kossen - 6-7 | 209 - 201 Ma Mesozoic | carbonate | 29 |
| Kossen - Hochalm | 209 - 201 Ma Mesozoic | carbonate, "limestone" | 71 |
| Kossen - Hochalm, Unit 3 | 209 - 201 Ma Mesozoic | carbonate | 7 |
| Kossen - Hochalm,Unit2 | 209 - 201 Ma Mesozoic | carbonate/marl, "carbonate", marl/"carbonate", marl | 130 |
| Kossen - Hochalm,Unit3 | 209 - 201 Ma Mesozoic | carbonate, "carbonate"/marl, marl/"carbonate", "carbonate"/claystone | 123 |
| Kossen - Holchalm, Unit 2 | 209 - 201 Ma Mesozoic | 4 | |
| Kossen - Holchalm, Unit 3 | 209 - 201 Ma Mesozoic | carbonate, marl | 8 |
Recorded Fossils
References
| Golebiowski R. (1989) Stratigraphie und Biofacies der Koessener Formation (Obertrias, Nordliche Kalkalpen), Ph.D. thesis, University of Vienna, Austria, 1-253 |
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!
