Where: Egypt (31.0° N, 33.5° E: paleocoordinates 7.1° N, 29.0° E)
• outcrop-level geographic resolution
When: Risan Aneiza Formation, Aptian (125.0 - 113.0 Ma)
• STRATIGRAPHIC RELATIONS: From lower 72 m of Risan Aneiza Formation, which underlies limestone of the Hala Fm (Cenomanian). THICKNESS: 414 m. AGE: Aptian based on multiple macrofossil biostratigraphic indicators.
• group of beds-level stratigraphic resolution
Environment/lithology: marine; poorly lithified, shelly/skeletal siltstone and poorly lithified, shelly/skeletal claystone
Size class: macrofossils
Collection methods: quarrying,
• COLLECTOR: Presumably collected by M.A. Abdelhamid during PhD research (1995). REPOSITORY: Geol. Dept., Fac. Science, Ain Shams University, Cairo.
Primary reference: M. A. Abdelhamid and M.M. Azab. 2003. Aptian-Cenomanian Echinoids from Egypt. Revue de Paleobiologie, Geneve 22(2):851-876 [A. Miller/A. Hendy]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 63979: authorized by Austin Hendy, entered by Austin Hendy on 29.08.2006
Creative Commons license: CC BY (attribution)
Taxonomic list
Echinoidea | |
Trochodiadema libanoticum sea urchin | |
Tetragramma barthouxi sea urchin | |
"Pseudodiadema julii" = Diplopodia (Pseudodiadema)
"Pseudodiadema julii" = Diplopodia (Pseudodiadema) sea urchin | |
Leptosalenia humei Fourtau 1921 sea urchin | |
Pseudoholaster barthouxi sea urchin | |
"Toxaster dieneri" = Pliotoxaster dieneri
"Toxaster dieneri" = Pliotoxaster dieneri de Loriol 1887 heart urchin | |
Cidaris dowsoni pencil urchin |