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Coon Creek Formation information


Coon Creek
Stratigraphic range: Early Maastrichtian
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
TypeFormation or member
OverliesSelma Chalk
Lithology
OtherLimestone, marl, sand, clay
Location
Coordinates34°24′N 88°54′W / 34.4°N 88.9°W / 34.4; -88.9
Approximate paleocoordinates38°00′N 66°12′W / 38.0°N 66.2°W / 38.0; -66.2
RegionCoon Creek Formation Tennessee, Coon Creek Formation Mississippi
CountryCoon Creek Formation USA
Type section
Named forCoon Creek (Mississippi)
Named byB. Wade

The Coon Creek Formation or Coon Creek Tongue is a geologic unit and Konservat-Lagerstätte located in western Tennessee and extreme northeast Mississippi.[1] It is a sedimentary sandy marl deposit, Late Cretaceous (Maastrichtian) in age, about 70 million years old. The formation is renowned for its pristine fossils of Late Cretaceous marine invertebrates, including gastropods, bivalves, decapod crustaceans, and ammonites, particularly at Coon Creek in McNairy County, Tennessee, which the formation is named for. It is also known for producing fosslis of marine vertebrates, such as mosasaurs and plesiosaurs. Notable fossils from this formation is the gastropod Turritella, the bivalve Pterotrigonia thoracica (the state fossil of Tennessee), as well as other fossils such as crabs.

It is alternately considered its own geologic formation (as the Coon Creek Formation) or a distinct member of the wider Ripley Formation (as the Coon Creek Member or the Coon Creek Tongue).[1][2]

  1. ^ a b "Geolex — CoonCreek". ngmdb.usgs.gov. Retrieved 2024-03-02.
  2. ^ Kornecki, Krystyna Maria (2014). Cretaceous confluence in the Coon Creek Formation (Maastrichtian) of Mississippi and Tennessee, USA: Taphonomy and systematic paleontology of a decapod konsentrat-lagerstätte (Thesis). OCLC 933765275.[page needed]

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