Where: Santander, Spain (43.5° N, 3.8° W: paleocoordinates 38.0° N, 4.7° W)
• coordinate estimated from map
When: Cabo de Lata Formation, Thanetian (59.2 - 56.0 Ma)
• Basal beds crossbedded calcarenites with manny hardgrounds and temporary hiatuses in sedimentation and were deposited during falling sea level,
Environment/lithology: marine; lithified, glauconitic limestone
Size classes: macrofossils, mesofossils
Preservation: cast
Reposited in the BMNH
• Echinodids only, collected from Site 10 of the Cabo Mayor collection
Primary reference: A. B. Smith, J. GallemÃ, C. H. Jeffery, G. Ernst, and P. D. Ward. 1999. Late Cretaceous-early Tertiary echinoids from northern Spain: implications for the Cretaceous-Tertiary extinction event. Bulletin of the Natural History Museum, London (Geology) 55(2):81-137 [P. Wagner/P. Wagner/P. Wagner]more details
Purpose of describing collection: biostratigraphic analysis
PaleoDB collection 157012: authorized by Melanie Hopkins, entered by Shaun Mahmood on 04.06.2014
Creative Commons license: CC BY (attribution)
Taxonomic list
Echinoidea | |
Gitolampas subrotundus sea urchin |