Bank der kleinen Terebrateln, Upper Muschelkalk, Schwabish Hall: Ladinian, Germany
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Rhynchonellata
- Terebratulida
- Dielasmatidae
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Coenothyris sp.
Douvillé 1879
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Polychaeta
- Sabellida
- Serpulidae
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Spirorbis sp.
Daudin 1800
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Gastropoda
- Acteoninidae
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Actaeonina sp.
(d'Orbigny 1850)
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original and current combination Acteonina | |||||||
Gastropoda
- Neritariidae
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"Neritaria" sp.
Koken 1892
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Gastropoda
- Murchisoniina
- Loxonematidae
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Loxonema sp.
Phillips 1841
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Bivalvia
- Nuculida
- Nuculidae
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Palaeonucula sp.
Quenstedt 1930
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Bivalvia
- Ostreida
- Bakevelliidae
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Hoernesia sp.
Laube 1865
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Bivalvia
- Pectinida
- Pectinidae
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Pleuronectites sp.
Schlotheim 1820
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Bivalvia
- Pectinida
- Anomiidae
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Placunopsis sp.
Morris and Lycett 1853
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Bivalvia
- Pectinida
- Limidae
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Plagiostoma sp.
Sowerby 1814
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Bivalvia
- Trigoniida
- Myophoriidae
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Myophoria sp.
Bronn 1834
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Bivalvia
- Pholadida
- Pleuromyidae
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Pleuromya sp.
(Meek 1873)
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original and current combination Myacites (Pleuromya) | |||||||
Bivalvia
- Carditida
- Myophoricardiidae
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Pseudocorbula sp.
Philippi 1898
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see common names |
Geography
Country: | Germany | State/province: | Baden-Wurttemberg |
Coordinates: | 49.2° North, 9.8° East (view map) | ||
Paleocoordinates: | 15.4° North, 17.8° East | ||
Basis of coordinate: | based on nearby landmark | ||
Geographic resolution: | local area |
Time
Period: | Triassic | Epoch: | Middle Triassic |
Stage: | Ladinian | 10 m.y. bin: | Triassic 2 |
Key time interval: | Ladinian | ||
Age range of interval: | 242.00000 - 237.00000 m.y. ago |
Stratigraphy
Geological group: | Muschelkalk | ||||
Stratigraphic resolution: | group of beds | ||||
Stratigraphy comments: Discoceratite Zone. 1.2-1.4 m thick. Upper Muschelkalk Subgroup |
Lithology and environment
Primary lithology: | concretionary,shelly/skeletal silty rudstone |
Lithology description: Irregularly bedded, nodular microsparitic biorudites with mud- and silt-streaks. In the lowest and uppermost parts of the unit, mudstone lenses reach several cm in thickness. These parts are characterized by strongly bioturbated, poorly sorted wackestones, whereas the middle part of the unit is dominated by packstones which show several levels with varying particle sizes and packing densities and are generally poor in mud. | |
Environment: | marine indet. |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Temporal resolution: | condensed |
Spatial resolution: | allochthonous |
Collection methods and comments
Collection methods: | field collection |
Reason for describing collection: | taphonomic analysis |
Metadata
Database number: | 44344 | ||
Authorizer: | D. Bottjer | Enterer: | M. Clapham |
Modifier: | M. Carrano | Research group: | marine invertebrate |
Created: | 2004-09-08 15:00:02 | Last modified: | 2022-11-09 15:14:33 |
Access level: | the public | Released: | 2004-09-08 15:00:02 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
11656. | H. Hagdorn. 1982. The "Bank der kleinen Terebrateln" (Upper Muschelkalk, Triassic) near Schwabisch Hall (SW Germany) - a tempestite condensation horizon. Cyclic and Event Stratification 263-285 [D. Bottjer/M. Clapham/M. Clapham] |