Danata Formation
| Danata Formation | |
|---|---|
| Stratigraphic range: Early Eocene-Mid Eocene ~ | |
| Type | Geological formation |
| Location | |
| Coordinates | 38°38′N 55°48′E / 38.633°N 55.800°E[1] |
| Approximate paleocoordinates | 35°06′N 51°12′E / 35.1°N 51.2°E |
| Country | File:Flag of Turkmenistan.svg Turkmenistan |
Danata Formation (Turkmenistan) | |
The Danata Formation (or Danatinskaya, Danatinsk, Russian: Danata Svita) is an earliest Eocene to Middle Eocene sedimentary succession located in Turkmenistan. It is mostly famous for its fish-bearing horizons (Ichthyofauna).[1] The formation for example crops out in the Kopet Dag mountain range in the border region of Turkmenistan and Iran.[1] It was deposited in a far northeastern arm of the Tethys Sea.[2] Previously, it was thought that the earliest horizons of this formation dated to the latest Paleocene (Thanetian). However, more recent studies have found the formation's sapropel to originate from a global anoxic event caused by the Paleocene-Eocene Thermal Maximum, indicating that it formed just after the Paleocene-Eocene boundary, during the earliest Ypresian.[2]
Paleoenvironment
The Danata Formation is famous for its ichthyofauna. The fish are found in a 9 metres (30 ft) thick clay horizon in the middle of the succession, that has been dated as earliest Ypresian, around 56 million years ago.[1][2] This includes fossils of the family Turkmenidae. Luvarus necopinatus was first described in this formation. Other fossils of fish include the genera Eospinus, Danatinia, Exellia, Turkmene and Avitoluvarus. The snake species Archaeophis turkmenicus has also been described.[3] A similar fauna occurs in the Moler Formation in Denmark.[1] The majority of these taxa were named by prominent Russian ichthyologist Pavel Daniltshenko.[4] The fauna is largely dominated by three species: Primisardinella genetrix, Chanos torosus, and Mene triangulum. The formation appears to have been deposited in an open-water environment as the vast majority of genera had a pelagic lifestyle, with only two very rare benthic genera (Eolamprogrammus and Asanoa) known. Despite some of the similarities in the taxonomic affiliation of the Danata ichthyofauna with modern-day marine ichthyofauna, only five to six genera represented in the formation (Chanos, Seriola, Luvarus, Mene, Scomberomorus, and possibly Caesio) also have modern representatives. Uniquely, a high diversity of luvarid fishes is known from the formation, despite this family being represented by a single, very rare species (the louvar) in the modern day.[5]
Paleobiota
The following taxa are known:[4][5]
Bony fish
Reptiles
| Genus | Species | Notes | Image |
|---|---|---|---|
| "Archaeophis" | "A." turkmenicus | A palaeophiid snake. Assignment to Archaeophis disputed.[6] |
References
- ↑ 1.0 1.1 1.2 1.3 1.4 Prokofiev, Artém M. "The Late Paleocene fish fauna of Turkmenistan" (PDF). Archived from the original (PDF) on 15 March 2016. Retrieved 15 November 2013.
- ↑ 2.0 2.1 2.2 Bannikov, A. F.; Erebakan, I. G. (2023-10-01). "On the Evolution of Some Groups of Marine Bony Fishes in the Cenozoic of the Tethys and Paratethys". Paleontological Journal. 57 (5): 475–490. Bibcode:2023PalJ...57..475B. doi:10.1134/S0031030123050015. ISSN 1555-6174.
- ↑ Head et al., 2005
- ↑ 4.0 4.1 Bannikov, A. F.; Parin, N. N. (1996). "The List of Marine Fishes From Cenozoic (Upper Paleocene-Middle Miocene) Localities in Southern European Russia and Adjacent Countries". Voprosy Ikhtiologii. 37 (2): 149–161.
- ↑ 5.0 5.1 Банников, Александр Федорович (2009). "Ископаемые колючеперые рыбы (Acanthopterygii): систематика, филогения и роль в кайнозойских ихтиокомплексах Тетиса и Паратетиса". Палеонтология и стратиграфия (in русский).
- ↑ Gower, David J.; Zaher, Hussam (2022-08-11). The Origin and Early Evolutionary History of Snakes. Cambridge University Press. ISBN 978-1-108-94507-3.
Bibliography
- Head, Jason J.; Holroyd, Patricia A.; Hutchison, J. Howard; Ciochon, Russell L. (2005), "First report of snakes (Serpentes) from the Late Middle Eocene Pondaung Formation, Myanmar", Journal of Vertebrate Paleontology, 25 (1): 246–250, doi:10.1671/0272-4634(2005)025[0246:FROSSF]2.0.CO;2