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Middle Kimmeridge marls, Bad Harzburg, Goslar District, Lower Saxony, Germany
| Formation | Middle Kimmeridge marls |
|---|---|
| Age: | 157 - 152 Ma Jurassic |
| Interval | Kimmeridgian |
| Lithology | marl, "limestone", lime mudstone/marl |
| Number of Collections | 14 |
| Number of Occurrences | 50 |
Recorded Sample Locations
| Location | Region | Stratigraphic Name |
|---|---|---|
| Rohstoffbetriebe Oker quarry | Bad Harzburg, Goslar District, Lower Saxony, Germany | Middle Kimmeridge marls |
Associated Units
| Stratigraphic Name | Age | Lithology | Occurrence Records |
|---|---|---|---|
| Lower Kimmeridge marls | 157 - 152 Ma Jurassic | marl | 56 |
| Upper Kimmeridge marls | 157 - 152 Ma Jurassic | marl | 8 |
Recorded Fossils
| Accepted Name | Hierarchy | Age |
|---|---|---|
 Coleopteraorder | Animalia : Arthropoda : Insecta : Coleoptera | 157.3 - 152.1 Ma Jurassic |
 Hybodontoideasuperfamily | Animalia : Chordata : Chondrichthyes : Hybodontiformes : Hybodontoidea | 157.3 - 152.1 Ma Jurassic |
 Neoselachiiunranked clade | Animalia : Chordata : Chondrichthyes : Neoselachii | 157.3 - 152.1 Ma Jurassic |
| Rhinobatoidei suborder | Animalia : Chordata : Chondrichthyes : Rajiformes : Asterodermus : Rhinobatoidei | 157.3 - 152.1 Ma Jurassic |
| Galeomorphi superorder | Animalia : Chordata : Chondrichthyes : Selachii : Galeomorphi | 157.3 - 152.1 Ma Jurassic |
| Palaeospinacidae family | Animalia : Chordata : Chondrichthyes : Synechodontiformes : Palaeospinax : Palaeospinacidae | 157.3 - 152.1 Ma Jurassic |
| Synechodus sp. genus | Animalia : Chordata : Chondrichthyes : Synechodontiformes : Palaeospinacidae : Synechodus | 157.3 - 152.1 Ma Jurassic |
 Eucryptodiraunranked clade | Animalia : Chordata : Reptilia : Testudines : Eucryptodira | 157.3 - 152.1 Ma Jurassic |
References
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!
