1km east of Ain Murun: Late Cenomanian, Egypt
collected by R. Markgraf 1922
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Chondrichthyes
- Hybodontiformes
- Acrodontidae
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see common names |
Geography
Country: | Egypt |
Coordinates: | 28.4° North, 28.9° East (view map) |
Paleocoordinates: | 12.9° North, 34.8° East (Wright 2013) |
Basis of coordinate: | based on nearby landmark |
Geographic resolution: | outcrop |
Time
Period: | Cretaceous | Epoch: | Late Cretaceous |
Stage: | Cenomanian | 10 m.y. bin: | Cretaceous 5 |
Key time interval: | Late Cenomanian | ||
Age range of interval: | 100.5 - 93.9 m.y. ago |
Stratigraphy
Formation: | Bahariya | Member: | Gebel Dist | ||
Stratigraphic resolution: | group of beds | ||||
Stratigraphy comments: Dominik (1985) reported the early Late Cenomanian ammonite Neolobites vibrayeanus from both the Gebel Dist Member (upper part) and the El Heiz Member (now Formation), confirmed by Wiese & Schulze, 2005 in their review of north African Neolobites. Malchus (1990) also compared the oysters from throughout the Gebel Dist Member with ones from the Egyptian eastern desert, dated by good ammonite age control as early Late Cenomanian. |
Lithology and environment
Primary lithology: | lithified sandy claystone |
Environment: | marginal marine indet. |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Collection methods and comments
Reason for describing collection: | taxonomic analysis | ||
Museum repositories: | BSP | ||
Collectors: | R. Markgraf | Collection dates: | 1922 |
Metadata
Database number: | 214434 | ||
Authorizer: | M. Clapham | Enterer: | M. Clapham | Research group: | vertebrate |
Created: | 2020-09-30 00:12:30 | Last modified: | 2025-02-22 15:12:02 |
Access level: | the public | Released: | 2020-09-30 00:12:30 |
Creative Commons license: | CC0 |
Reference information
Primary reference:
73936. | E. Stromer. 1927. Ergebnisse der Forschungsreisen Prof. E. Stromers in den Wüsten Ägyptens II. Wirbeltier-Reste der Baharîje-Stufe (unterstes Cenoman) 9. Die Plagiostomen, mit einem Anhang über käno- und mesozoische Rückenflossenstacheln von Elasmobranchiern. Abhandlungen der Bayerischen Akademie der Wissenschaften, Mathematisch-Naturwissenschaftliche Abteilung 31(5):1-64 [M. Clapham/M. Clapham] |