Where: Egypt (30.1° N, 31.1° E: paleocoordinates 11.4° N, 25.9° E)
• coordinate estimated from map
• outcrop-level geographic resolution
When: Rudist Member (middle Abu Roash Formation), Middle Turonian (93.5 - 89.3 Ma)
Environment/lithology: sand shoal; limestone and rudstone
•marl interbeds. Bioclasts commonest components; followed by moderately sorted intraclasts. Lower contact sharp, upper one gradational. Mollusks, echinoid, and sponge fragments. Intraclasts, quartz grains, and grain aggregates occur. Rudist bivalves predominate.
Size classes: macrofossils, mesofossils
Primary reference: A. A. Abdelhady and R. S. A. Mohamed. 2017. Paucispecific macroinvertebrate communities in the Upper Cretaceous of El Hassana Dome (Abu Roash, Egypt): Environmental controls vs adaptive strategies. Cretaceous Research 74:120-136 [W. Kiessling/M. Krause/M. Uhen]more details
Purpose of describing collection: paleoecologic analysis
PaleoDB collection 184737: authorized by Wolfgang Kiessling, entered by Mihaela Krause on 21.03.2017
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Porifera indet. Grant 1836 | |
Gastropoda | |
Gastropoda indet. Cuvier 1795 snail | |
Bivalvia | |
"Durania arnaudi" = Durania cornupastoris
"Durania arnaudi" = Durania cornupastoris Des Moulins 1826 rudist | |
Bryozoa | |
Bryozoa indet. bryozoan | |
Echinoidea | |
Echinoidea indet. Leske 1778 sea urchin |