Bladen Formation | |
---|---|
Stratigraphic range: Middle Campanian ~ | |
Type | Formation |
Unit of | Black Creek Group |
Underlies | Donoho Creek Formation, Peedee Formation |
Overlies | Tar Heel/Coachman Formation |
Lithology | |
Primary | Sandstone, siltstone |
Location | |
Region | North Carolina South Carolina |
Country | United States |
Type section | |
Named for | Bladen County, North Carolina |
The Bladen Formation is a geologic formation from the Late Cretaceous (middle Campanian) of North Carolina and South Carolina, USA. It is known for a plethora of terrestrial and aquatic vertebrate fossils, including dinosaurs and mosasaurs.[1] It appears to be roughly concurrent with the Tuscaloosa Formation of Alabama.[2]
Unlike many other Cretaceous geologic formations from eastern North America, which were deposited in entirely marine environments, the Bladen Formation appears to have been deposited in a former river delta in an estuarine habitat, allowing for a mixture of freshwater, terrestrial, and marine fauna.[3] An important locality is the former Bladen County landfill annex in Elizabethtown, North Carolina, which contains the richest known fauna from the formation.[4][5] Another notable locality is near Quinby in Florence County, South Carolina, which also appears to have been deposited in a nonmarine environment with minor marine influence.[6]
It is deposited as a thin layer over the Tar Heel/Coachman Formation, which is often confused with. In North Carolina, it underlies the Maastrichtian-aged Peedee Formation, while in South Carolina it underlies the slightly younger Campanian-aged Donoho Creek Formation.[7]