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Kecskehát Limestone

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Geologic formation in Hungary
Kecskehát Limestone
Stratigraphic range: Pliensbachian
~184 Ma PreꞒ O S D C P T J K Pg N
TypeGeological formation
Unit ofTisza Unit
OverliesMecsek Coal Formation
Lithology
PrimaryModified grain flow sediment; coarse-grained crinoidal limestone
OtherSandstone
Location
RegionKecskemét
Country Hungary
Type section
Named forKecskehát caves

The Kecskehát 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.

Vertebrate paleofauna

Dinosaurs

Indeterminate sauropod remains once misattributed to the Cetiosauridae are present in the province of Kecskemét, Hungary.

Dinosaurs of the Kecskehát Limestone
Genus Species Location Stratigraphic position Material Notes Images
Mamenchisauridae Indeterminate new species
  • Skull
  • Vertebrae
  • Femur
  • Tibia
  • Isolated teeth
An indeterminate sauropod related to the Mamenchisauridae, with a similar build to Omeisaurus
Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

See also

References

  1. 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.
  2. 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 .
  3. 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


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