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The location of the state of Tennessee. Paleontology in Tennessee refers to paleontological research occurring within or conducted by people from the U.S. state of Tennessee. During the early part of the Paleozoic era, Tennessee was covered by a warm, shallow sea. This sea was home to brachiopods, bryozoans, cephalopods, corals, and trilobites.
The Tennessee Division of Archaeology maintains a database of all archaeological sites recorded within the state of Tennessee. As of January 1, 2009 this catalog contains more than 22,000 sites, including both prehistoric and historic resources.
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 ...
This list of the Paleozoic life of Tennessee contains the various prehistoric life-forms whose fossilized remains have been reported from within the US state of Tennessee and are between 538.8 and 252.17 million years of age.
Fossil of the Middle-Late Ordovician giant trilobite Isotelus. †Isotelus †Kockelella †Krausella †Lingulella †Lonchodomas †Marsupiocrinus †Meristella †Meristina †Monomorphichnus †Orthoceras †Ozarkodina †Ozarkodina confluens †Paciphacops; Fossilized theca of the Carboniferous blastoid echinoderm ("sea bud") Pentremites ...
Dunbar Cave State Park: Montgomery County: 8.067 miles (12.983 km) Forbidden Caverns: Sevier County: 0.5 miles (0.80 km) c. 1920 Hubbard's Cave: Warren County: 1810 [11] Largest gray bat hibernaculum in Tennessee. [12] Lookout Mountain Caverns: Hamilton County: 12 miles (19 km) 1823 No longer accessible since 2005. [13] Connected to Ruby Falls ...
The science center is situated on a 232 acres (94 ha) property on one of the most important fossil sites in North America. [1] The Coon Creek Formation is a geologic formation located in western Tennessee and extreme northeast Mississippi. It is a sedimentary sandy marl deposit, Late Cretaceous in age, about 73 million years old.
Dinosaur and mosasaur remains are among the fossils that have been recovered from the Selma Group. [1] [2] Oil was discovered in 1939 within the Late Cretaceous Woodruff Sandstone within the Selma Chalk Formation. Known as Mississippi's first oil field, the Tinsley Oil Field is located adjacent to Tinsley, Mississippi. [3]
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