Where: Santander, Spain (43.5° N, 3.8° W: paleocoordinates 35.7° N, 3.0° W)
• coordinate estimated from map
When: Cabo de Lata Formation, Maastrichtian (72.1 - 66.0 Ma)
• Basal beds crossbedded calcarenites with manny hardgrounds and temporary hiatuses in sedimentation and were deposited during falling sea level,
Environment/lithology: marine; lithified, sandy limestone
Size classes: macrofossils, mesofossils
Preservation: cast
Reposited in the BMNH
• Echinodids only, collected from Site 4 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 157006: authorized by Melanie Hopkins, entered by Shaun Mahmood on 04.06.2014
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Echinoidea | |
Phymosoma hexaporum sea urchin | |
Salenia scabra sea urchin
Salenia sp. Gray 1835 sea urchin | |
Echinogalerus muelleri sea urchin
? Echinogalerus vetschauensis sea urchin | |
Camerogalerus cantabrius sea urchin | |
Zuffardia sp. Checchia-Rispoli 1917 sand dollar | |
"Rhynchopygus sp." = Cassidulus (Rhynchopygus) d'Orbigny 1856 sea urchin
Nucleopygus coravium sea urchin
Nucleopygus scrobiculatus Goldufss 1826 sea urchin | |
Hemipneustes sp. sea urchin | |
Hemiaster prunella Lamarck 1816 heart urchin | |
Conulus gigas sea urchin | |
Tylocidaris trempinus pencil urchin |