Where: Falcon, Venezuela (11.9° N, 70.0° W: paleocoordinates 11.2° N, 66.7° W)
• coordinate estimated from map
When: Cantaure Formation, Burdigalian (20.4 - 16.0 Ma)
• The base of the unit is a Balanus bed containing blocks of granite, passing upwards through sands and calcareous sands. The top of the Cantaure Formation is conformably overlain by limestone layers that have been interpreted by Jung (1965) and Hunter and Bartok (1974) as post-Cantaure and pre-Pliocene sedimentation. Rey (1996) suggested that the upper contact of the Cantaure Formation represents an unconformity with the Amuay Member (early Pliocene) of the Paraguaná Formation. (Landau and Vermeij 2010; Carrillo-Briceño et al., 2016).
Environment/lithology: marginal marine; silty shale and medium-grained, silty sandstone
Size class: macrofossils
Primary reference: O. Aguilera, D. Rodrigues de Aguilera, F. J. Vega and M. R. Sanchez-Villagra. 2010. Mesozoic and Cenozoic decapod crustaceans from Venezuela and related trace-fossil assemblages. In M. R. Sanchez-Villagra, O. A. Aguilera, A. A. Carlini (eds.), Urumaco and Venezuelan Paleontology: The Fossil Record of the Northern Neotropics 103-129 [J. Wolfe/A. Lynch]more details
Purpose of describing collection: general faunal/floral analysis
PaleoDB collection 228724: authorized by Joanna Wolfe, entered by Arthur Lynch on 29.12.2022
Creative Commons license: CC BY (attribution)
Taxonomic list
Malacostraca | |
Eoinachoides sp. Van Straelen 1933 spider crab | |
Parthenope sp. Weber 1795 crab | |
Eriosachila sp., "Hepatella amazonica" = Miohepatus amazonicus
Eriosachila sp. Blow and Manning 1996 crab
"Hepatella amazonica" = Miohepatus amazonicus Beurlen 1958 crab | |
Calappa sp. Weber 1795 box crab | |
Iliacantha sp. Stimpson 1871 crab | |
Portunus oblongus Rathbun 1920 swimming crab
Saratunus sp. Collins et al. 2003 swimming crab | |
Paguristes sp. Dana 1851 hermit crab | |
Petrochirus sp. Stimpson 1858 hermit crab |