| 词条 | Curré Formation |
| 释义 |
| name = Curré Formation | image = | caption = | type = Formation | age = Hemphillian | period = Messinian | prilithology = Conglomerate | otherlithology = | namedfor = Rey Curré | namedby = | region = Limón & Puntarenas Provinces | country = {{CRI}} | coordinates = {{coord|8.9|N|83.1|W|display=inline,title}} | paleocoordinates = {{coord|8.8|N|83.1|W|display=inline}} | unitof = Taraba Basin Group | subunits = | underlies = | overlies = | thickness = | extent = Taraba Basin | area = | map = {{Location map+ | Costa Rica | relief = 1 | width = 250 | float = center | places = | lat_deg = 8.9 | lon_deg = -83.1 | mark = Yellow pog.svg | marksize = 12 }} | map_caption = }} The Curré Formation is a geologic formation of the Taraba Basin Group in Costa Rica. The deltaic conglomerates preserve fossils dating back to the Late Miocene to Early Pliocene period (Hemphillian).[1] Fossil contentThe following fossils have been found in the formation: {{div col|colwidth=20em}}
See also{{Portal|Earth sciences|Costa Rica|Paleontology|Neogene|Prehistory of North America}}
References1. ^Curré Formation at Fossilworks.org Further reading
8 : Geologic formations of Costa Rica|Neogene Costa Rica|Hemphillian|Conglomerate formations|Deltaic deposits|Paleontology in Costa Rica|Geography of Limón Province|Geography of Puntarenas Province |
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