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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.
List of the Paleozoic life of Tennessee. 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 ...
In Tennessee, Prehistoric is generally defined as the time between the appearance of the first people in the region (c. 12,000 BC) and the arrival of the first European explorers (c. 1540 AD). The Historic period begins after the arrival of those Europeans and continues to the present.
The Gray Fossil Site is an Early Pliocene assemblage of fossils dating between 4.5 and 4.9 million years old, located near the community of Gray in Washington County, Tennessee. The site was discovered during road construction on Tennessee State Route 75 by the Tennessee Department of Transportation in May 2000, [1] after which local officials ...
Florida: There is no state fossil in Florida, though agatised coral, which is a fossil, is the state stone. Hawaii. Iowa: The crinoid was proposed in 2018. [2] Minnesota: The giant beaver was proposed in 2022. [3] New Hampshire: The American mastodon (Mammut americanum) was considered in 2015.
Coon Creek (Mississippi) Named by. B. 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.
This page was last edited on 7 September 2020, at 12:43 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike License 4.0; additional terms may apply.