Where: Cienfuegos, Cuba (22.3° N, 80.2° W: paleocoordinates 19.5° N, 61.4° W)
• coordinate stated in text
• small collection-level geographic resolution
When: Monos Formation, Late/Upper Campanian to Late/Upper Campanian (83.5 - 66.0 Ma)
• The Monos Formation was deposited during part of a transgressive cycle characterized by a sequence of polymictic gravels that transition into sandstones originated by the erosion of the Antillean Cretaceous Volcanic Arc. Simultaneously, siltstone, claystone, and calcareous beds can also be found intercalated in some sections. These clastic sediments were deposited in a post-volcanic basin during the upper Campanianelower Maastrichtian (Iturralde-Vinent, 2014).
• group of beds-level stratigraphic resolution
Environment/lithology: fluvial; mudstone
Size class: macrofossils
Collection methods: The specimens here described are housed at the Museo Municipal de Rodas (MMR) in Rodas, Cienfuegos, Central Cuba.
Primary reference: L. W. Viñola-López, A. Cerda, J. Correa-Narvaez, L. Codorniú, C. R. Borges-Sellén, A. F. Arano-Ruiz, and Y. Ceballos-Izquierdo. 2022. New fossils shed light on the Late Cretaceous terrestrial community in the Caribbean and the First American Biotic Interchange. Cretaceous Research 130:105067 [P. Mannion/G. Varnham/P. Mannion]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 225169: authorized by Philip Mannion, entered by Grace Varnham on 28.04.2022
Creative Commons license: CC BY (attribution)
Taxonomic list
Sedentaria | |
Polychaeta | |
Scaphopoda | |
Dentalium sp. Linnaeus 1758 tusk shell | |
Bivalvia | |
Inoceramus sp. Sowerby 1814 clam | |
Angiospermae | |
|