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Belgrade Formation

Geologic formation in North Carolina, United States From Wikipedia, the free encyclopedia

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The Belgrade Formation is a limestone geologic formation in North Carolina characterized by limestone coquina mixed with sand, and thinly laminated clays.[2] It preserves fossils dating back to the Paleogene period.

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Description

The Belgrade Formation is composed of two subunits: the Pollocksville member and the Haywood Landing member. The Pollocksville member is composed of unconsolidated oyster shells and sand. It was deposited in the Oligocene and early Miocene. The Haywood Landing member is composed of shelly sands and thinly laminated clays. The Belgrade Formation was originally considered part of an Eocene formation called the Trent Marl before it was identified as being deposited in the Miocene and split off.[2]

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Fossil content

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Mammals

More information Carnivorans, Genus ...
More information Cetaceans, Genus ...
More information Sirenians, Genus ...

Reptiles

More information Reptiles, Genus ...

Fish

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Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
More information Chondrichthyes, Genus ...
More information Osteichthyes, Genus ...

Invertebrates

More information Molluscs, Genus ...
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References

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