The Tuscahoma Formation or Tuscahoma Sand is a geologic formation in Mississippi and Alabama, USA. It preserves fossils dating back to the early Paleogene period, from the Late Paleocene and Early Eocene.[1] It was primarily deposited in a marine habitat, but one Wasatchian-aged locality near Meridian, Mississippi was deposited in an estuarine habitat that preserves a significant terrestrial vertebrate fauna, known as the "Red Hot local fauna".[2][3] It preserves one of the most diverse early Eocene mammalian faunas from eastern North America, roughly contemporaneous with the Willwood Formation of Wyoming.[3][4]
Tuscahoma Formation | |
---|---|
Stratigraphic range: Thanetian to earliest Ypresian, | |
Type | Formation |
Unit of | Wilcox Group |
Sub-units | Bells Landing Member, Greggs Landing Member |
Underlies | Bashi Formation |
Overlies | Nanafalia Formation |
Lithology | |
Primary | Sandstone |
Location | |
Region | Mississippi, Alabama |
Country | United States |
Vertebrate paleofauna
editRay-finned fishes
editBased on the Paleobiology Database:[5]
Ray-finned fishes of the Tuscahoma Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Albula | A. eppsi | Lauderdale County, Mississippi | Early Eocene | A bonefish. | ||
A. oweni | ||||||
Brychaetus | B. muelleri | A bonytongue. | ||||
Egertonia | E. isodonta | A phyllodontid. | ||||
Lepisosteus | L. sp. | A gar. Assigned to the European species L. suessionensis (itself a junior synonym of L. fimbriatus), but this is unlikely due to their differring ranges.[6] | ||||
Palaeocybium | P. proosti | A mackerel. | ||||
Phyllodus | P. toliapicus | A phyllodontid. | ||||
Pycnodus | P. bowerbanki | A pycnodont. | ||||
Trichiurides | T. sagittidens | A cutlassfish. |
Reptiles
editBased on the Paleobiology Database:[4][7]
Reptiles of the Tuscahoma Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Palaeophis | P. casei | Meridian, Mississippi | Early Eocene | A marine palaeophiid snake. | ||
P. littoralis | ||||||
P. virginianus | ||||||
Tuscahomaophis | T. leggetti | Late Paleocene | An alethinophidian snake. |
Mammals
editThe Tuscahoma Formation preserves a diversity of earliest Eocene-aged mammals. Almost all mammals are known only from isolated teeth. There appear to be significant differences in the faunal composition between the Tuscahoma Formation and the contemporaneous Bighorn Basin of the western US, indicating some level of provincialism in North American mammal species assemblages of the time. The formation appears to have been biased against the preservation of large-sized mammals, meaning that the majority of mammal remains from the formation are of smaller taxa.[3]
Based on the Paleobiology Database and Dawson & Beard (2009):[4][3]
Metatheria
editMetatherians of the Tuscahoma Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Mimoperadectes | M. sowasheensis | Meridian, Mississippi | Early Eocene | A peradectid. | ||
Peratherium | P. mcgrewi | A herpetotheriid. |
Cimolesta
editCimolestans of the Tuscahoma Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Coryphodon | C. sp. | Meridian, Mississippi | Early Eocene | A pantodont. | ||
Naranius | N. americanus | A cimolestid. Type locality of species. | ||||
Palaeosinopa | P. aestuarium | A pantolestid. Type locality of species. |
Macroscelidea
editMacroscelideans of the Tuscahoma Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Haplomylus | H. meridionalis | Meridian, Mississippi | Early Eocene | An apheliscid. |
Ungulates
editUngulates of the Tuscahoma Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Diacodexis | D. sp. | Meridian, Mississippi | Early Eocene | An even-toed ungulate. | ||
Ectocion | E. nanabeensis | A phenacodont. Type locality of species. | ||||
Hyracotherium | H. sp. | An odd-toed ungulate. |
Pan-Carnivorans
editUngulates of the Tuscahoma Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Eogale | E. parydros | Meridian, Mississippi | Early Eocene | A miacid carnivoramorph. Type locality of genus and species. | ||
Gracilocyon | G. igniculus | A carnivoraform. | ||||
"Miacis" | "M." sp. | A carnivoramorph. | ||||
Prototomus | P. sp. | A sinopid hyaenodont. | ||||
Uintacyon | U. sp. | A carnivoraform. | ||||
Vassacyon | V. sp. | A carnivoraform. | ||||
Viverravus | V. laytoni | A viverravid carnivoramorph. | ||||
Viverriscus | V. omnivorus | A viverravid carnivoramorph. Type locality of genus and species. |
Eulipotyphlans
editEulipotyphlans of the Tuscahoma Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Colpocherus | C. mississippiensis | A sespedectid. Type locality of genus and species. | ||||
Diacocherus | D. dockeryi | An erinaceoid. Type localiy of species. | ||||
Plagioctenodon | P. dormaalensis | A nyctitheriid. | ||||
Talpavoides | T. dartoni | A stem-erinaceid.[8] | ||||
Wyonycteris | W. primitivus | A nyctitheriid. Type locality of species. |
Apatotherians
editApatotherians of the Tuscahoma Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Apatemys | A. pygmaeus | Meridian, Mississippi | Early Eocene | An apatemyid. Type locality of species. |
Rodents
editRodents of the Tuscahoma Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Corbarimys | C. nomadus | Meridian, Mississippi | Early Eocene | An ischyromyoid.[9] | ||
Franimys | F. actites | An ischyromyid. | ||||
Paramys | P. dispar | An ischyromyid. | ||||
Tuscahomys | T. major | A cylindrodontid. Type locality of genus and species. | ||||
T. medius | ||||||
T. minor |
Primates
editPrimates of the Tuscahoma Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Choctawius | C. foxi | Meridian, Mississippi | An omomyid. Type locality of genus and species. | |||
Teilhardina | T. magnoliana | An omomyid. |
See also
editReferences
edit- ^ "Geolex — Tuscahoma publications". ngmdb.usgs.gov. Retrieved 2024-11-21.
- ^ "PBDB Collection". paleobiodb.org. Retrieved 2024-11-21.
- ^ a b c d Beard, K. Christopher; Dawson, Mary R. (2009). "Early Wasatchian Mammals of the Red Hot Local Fauna, Uppermost Tuscahoma Formation, Lauderdale County, Mississippi". Annals of Carnegie Museum. 78 (3): 193–243. doi:10.2992/007.078.0301. ISSN 0097-4463.
- ^ a b c "PBDB Collection". paleobiodb.org. Retrieved 2024-12-10.
- ^ "PBDB Collection". paleobiodb.org. Retrieved 2024-12-10.
- ^ Weems, Robert E. (1998). "Actinopterygian Fish Remains from the Paleocene of South Carolina". Transactions of the American Philosophical Society. 88 (4): 147–164. doi:10.2307/1006672. ISSN 0065-9746.
- ^ "PBDB Collection". paleobiodb.org. Retrieved 2024-12-10.
- ^ Vitek, Natasha S.; Morse, Paul E.; Boyer, Doug M.; Strait, Suzanne G.; Bloch, Jonathan I. (2021). "Evaluating the responses of three closely related small mammal lineages to climate change across the Paleocene–Eocene thermal maximum". Paleobiology. 47 (3): 464–486. doi:10.1017/pab.2021.12. ISSN 0094-8373.
- ^ Vianey-Liaud, Monique; Marivaux, Laurent (20 September 2021). "The beginning of the adaptive radiation of Theridomorpha (Rodentia) in Western Europe: morphological and phylogenetic analyses of early and middle Eocene taxa; implications for systematics". Palaeovertebrata. 44 (2): e2. doi:10.18563/pv.44.2.e2. ISSN 0031-0247. OCLC 9257882797. Retrieved 26 July 2024.
- Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.