Earth:Kcskehát Limestone
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Revision as of 11:43, 18 August 2022 by imported>QCDvac (fix)
Short description: Geologic formation in Hungary
| Kcskehát Limestone Stratigraphic range: Pliensbachian ~184 Ma | |
|---|---|
| Type | Geological formation |
| Unit of | Tisza Unit |
| Overlies | Mecsek Coal Formation |
| Lithology | |
| Primary | Modified grain flow sediment; coarse-grained crinoidal limestone[1] |
| Other | Sandstone |
| Location | |
| Region | Kecskemét |
| Country |  Hungary |
| Type section | |
| Named for | Kcskehát caves |
The Kcskehát Limestone is a Jurassic geologic formation in Hungary. Indeterminate fossil Sauropod tracks have been reported from the formation. It is abundant on Illite and very little Kaolinite that indicates a change from the humid-subtropical climate of the Mecsek Coal Formation to the monsoon-like semi-arid climate of the Pliensbachian formations. The dominance of illite indicates a relatively fast erosion of the source area and a moderate input of terrigenous clastics relative to the underlying formations.[2][3]
Vertebrate paleofauna
Dinosaurs
Indeterminate sauropod remains once misattributed to the Cetiosauridae are present in the province of Kecskemét, Hungary.[citation needed]
| Dinosaurs of the Kcskehát Limestone | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Mamenchisauridae | Indeterminate new species[citation needed] |
|
An indeterminate sauropod related to the Mamenchisauridae, with a similar build to Omeisaurus[citation needed] | |||
See also
- List of dinosaur-bearing rock formations
References
- ↑ Raucsik, B., & Varga, A. (2008). Climato-environmental controls on clay mineralogy of the Hettangian–Bajocian successions of the Mecsek Mountains, Hungary: an evidence for extreme continental weathering during the early Toarcian oceanic anoxic event. Palaeogeography, Palaeoclimatology, Palaeoecology, 265(1-2), 1-13.
- ↑ Császár G., Szinger B., Piros O. (2013) From continental platform towards rifting of the Tisza Unit in the late Triassic to Early Cretaceous. GeologicaCarpathica, 64: 279–290. Late Triassic climate humidification and kaolinite formation (Western Carpathians, Tatric Init of the Tatra Mts.) | Request PDF. Available from: https://www.researchgate.net/publication/259745031_Late_Triassic_cliamte_humidification_and_kaolinite_formation_Western_Carpathians_Tatric_Init_of_the_Tatra_Mts [accessed Aug 28 2018].
- ↑ Császár, G., Szinger, B., & Piros, O. (2013). From continental platform towards rifting of the Tisza Unit in the Late Triassic to Early Cretaceous. Geologica Carpathica, 64(4), 279-290.
Bibliography
- Weishampel, David B.; Peter Dodson, and Halszka Osmólska (eds.). 2004. The Dinosauria, 2nd edition, 1–880. Berkeley: University of California Press. Accessed 2019-02-21. ISBN:0-520-24209-2
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