Tallahatta Formation Fossil
Tallahatta Formation | |
---|---|
Age (Ma) | |
Start: | 47.8 |
End: | 41.3 |
System/Period: | Paleogene |
Series/Epoch: | Eocene |
Stage/Age: | Lutetian |
Location | |
Location: | Mississippi |
Country: | United States |
Coordinates: | 34.9°N, 89.3°W |
Paleocoordinates: | 36.2°N, 77.6°W |
Diversity | |
Genera: | 1 |
Bolden clay pit, northeast of Holly Springs, Mississippi, United States.
• 5 cm thick siltstone layer. Middle Eocene, Claibornian. Near the top of the Tallahatta Formation, just below the contact with the overlying Koscuisko Formation.
• bed-level stratigraphic resolution
Environment/lithology: pond; lithified siltstone
• The stratigraphic sequence at this locality corresponds to the sedimentology and typical sequence of an abandoned stream meander that has formed an oxbow lake and subsequently filled with clay, silt, and organic matter.
Species known from Tallahatta Formation
A single undescribed species of Oecophylla is the only fossil ant currently known from this formation.
Location of Formation
References
- Johnston, J.E. 1993. Insects, spiders, and plants from the Tallahatta Formation (Middle Eocene) in Benton County, Mississippi. Mississippi Geology 14: 71–82.
- Perfilieva, K.S. 2021. Distribution and differentiation of fossil Oecophylla (Hymenoptera: Formicidae) species by wing imprints. Paleontological Journal 55(1), 76–89 (doi:10.1134/s003103012101010x).