Where: Matanzas, Cuba (22.5° N, 81.1° W: paleocoordinates 22.8° N, 76.9° W)
• coordinate based on nearby landmark
• outcrop-level geographic resolution
When: Colón Formation, Late/Upper Oligocene to Late/Upper Oligocene (28.4 - 16.0 Ma)
• The Colón Formation is conformably overlain by the Güines Formation, which crops out extensively in this area and is currently correlated with the Lagunitas Formation in central Cuba. (Orihuela et al., 2019). It is disconformally covered by the Canimar formation. (Lopez et al., 2019). Underlying Formation: It is unclear what the underlying formation is. Thickness: Core samples collected near this location suggest a maximum thickness no greater than 65 m, of which the upper 5–20 m is exposed at these quarries (Franco et al., 1992).
• group of beds-level stratigraphic resolution
Environment/lithology: platform or shelf-margin reef; lithified limestone
Size class: macrofossils
Collection methods: Repository: Museo Nacional de Historia Natural de Cuba (MNHNCu)
Primary reference: C. Varela and C. E. Schweitzer. 2011. New genus and new species of Portunidae Rafinesque, 1815 (Decapoda, Brachyura) from the Colon Formation, Cuba. Bulletin of the Mizunami Fossil Museum 37:13-16 [J. Wolfe/A. Lynch/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 228535: authorized by Joanna Wolfe, entered by Arthur Lynch on 12.12.2022, edited by Matthew Clapham
Creative Commons license: CC BY (attribution)
Taxonomic list
Malacostraca | |
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Paraeuphylax cubaensis n. gen. n. sp. Varela and Schweitzer 2011 swimming crab |