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Mauvilla Local Fauna
Stratigraphic range: Late Miocene,
Hemphillian 7.3–6.8 Ma
TypeLocal Fauna
UnderliesCitronelle Formation
Thickness60 metres (200 ft)
Lithology
Primarysand, clay
Location
RegionAlabama
Country United States
Type section
Named forMauvilla, Alabama

The Mauvilla Local Fauna (also referred as the Mobile Local Fauna) is a local fauna in Alabama, the fossils within the fauna date back to the Late Miocene. The sediment that makes up the locality where the fossils are found underlies the Citronelle Formation. The local fauna preserves a deltaic ecosystem mostly made up of terrestrial vertebrates though fragmentary fish and cetacean material is also found at the site.

Discovery and Naming

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The vertebrate material that makes up the local fauna was originally found by James E. Davis Jr. in the fall of 1966 within Chickasaw Creek. As the name suggests, the local fauna is found near Mauvilla, a town in southwestern Alabama. More specimens were collected by both Davis and his father only to be given to G. M. Lamb at the University of South Alabama who then sent the fossils to National Museum of Natural History where the were identified is the first Hemphillian mammals to be found in Alabama. Before the local fauna was given a name, fossils from the locality were referenced in 1971 by Isphoding and Lamb where they gave it the name "Moblie local fauna" though the name "Mobile" is already used in the form of a nearby formation. Between the 1960's and 1980's, multiple excavations had taken place which recovered hundreds of vertebrates fossils from these deposits. [1][2]

Lithology

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The Mauvilla local fauna is derived from a 60 m interval of alternating beds of sand and dark clay with the clay layers averaging 10 cm while the sand layers are discontinuous and average from 2-3 cm.[1] Though originally believed to be part of the middle Pliocene Citronelle Formation, it was later discovered that it was a part of a section of undifferentiated sediment underlying the Citronelle Formation; it is currently labeled as a part of ‘Ecor Rouge Sand’. The vertebrate material itself is located in the sand layers just above the clay. Based on this and the fauna within the locality, it has been suggested that the fossils were deposited during a flooding event within a deltaic floodplain.[2]

Paleobiota

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Actinopterygii

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Genus Species Notes Image
Aplodinotus[3] A. grunniens
Atractosteus[3] A. sp. cf. A. spatula
Ictalurus[3] I. spp
Lepisosteidae gen. et. sp. indet.[3]
Scombroidei indet.[4]
Teleostei gen. et. sp. indet.[3]

Artiodactyla

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Genus Species Notes Image
Gelocidae cf. Pseudoceras sp.[1]
Pediomeryx[1] P. sp
Pleiolama[1] P. cf. vera A medium-sized camelid known from dental and limb material found within the local fauna. The dental remains fall within the variation seen in P. vera.
Pomatodelphis[1] P. inaequalis
Prosthennops[1] P. cf. serus A tayassuid known from dental remains along with metatarsals found within the local fauna. Though the material is too fragmentary to make an exact assignment, they are more similar to P. serus when comparing it to other members of the family that would have been around at the time.
Synthetoceras[1] S. davisorum

Carnivora

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Genus Species Notes Image
Epicyon[1] E. cf. haydeni A canid known from a radius and phalanx found within the local fauna. Though shorter than other material assigned to E. haydeni, they do fall within the intraspecific variation of borophagine limbs.

Crocodilia

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Genus Species Notes Image
Crocodilia indet.[4]

Perissodactyla

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Genus Species Notes Image
Aphelops[1] A. mutilus
Cormohipparion[1] C. emsliei
Nannippus[1] N. aztecus
Neohipparion[1] N. eurystyle
Protohippus[1] P. gidleyi
Tapirus[1] T. sp
Teleoceras[1] T. sp

Proboscidea

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Genus Species Notes Image
Gomphotheriidae gen. & sp. indet.[1]

Testudines

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Genus Species Notes Image
Apalone[5] A. sp A trionychid that was originally described as Trionyx though is currently thought to be assignable to either the species A. spinifera or A. ferox.

Paleoenvironment

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Overall the environment of the Mauvilla local fauna is representative of a subtropical to tropical delta, comparable to the modern day delta a part of the Mobile river system. This environment would have been in the middle of the transition between a more brackish environment made up of marshes to one that is a completely fluvial environment.[4]

References

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  1. ^ a b c d e f g h i j k l m n o p q Hulbert, Richard C.; Whitmore, Frank C. (2006-06-01). "Late Miocene mammals from the Mauvilla local fauna, Alabama". Bulletin of the Florida Museum of Natural History. 46 (1): 1–28. doi:10.58782/flmnh.xcpo4034. ISSN 0071-6154.
  2. ^ a b Ebersole, Jun A.; Jacquemin, Stephen J. (2020-07-02). "A late Miocene (Hemphillian) freshwater fish (Osteichthyes) fauna from Mobile County, Alabama, USA". Historical Biology. 32 (6): 750–763. doi:10.1080/08912963.2018.1530995. ISSN 0891-2963.
  3. ^ a b c d e Ebersole, Jun A.; Jacquemin, Stephen J. (2020-07-02). "A late Miocene (Hemphillian) freshwater fish (Osteichthyes) fauna from Mobile County, Alabama, USA". Historical Biology. 32 (6): 750–763. doi:10.1080/08912963.2018.1530995. ISSN 0891-2963.
  4. ^ a b c ISPHORDING, WAYNE C.; LAMB, GEORGE M. (1971). "Age and Origin of the Citronelle Formation in Alabama". Geological Society of America Bulletin. 82 (3): 775. doi:10.1130/0016-7606(1971)82[775:aaootc]2.0.co;2. ISSN 0016-7606.
  5. ^ JASINSKI, STEVEN E. (2013). "Review of the fossil Trionychidae (Testudines) from Alabama, including the oldest record of trionychid turtles from eastern North America". Bulletin of the Alabama Museum of Natural History. 31 (2).