Kecskehát Limestone | |
---|---|
Stratigraphic range:
Pliensbachian ~ | |
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 | Kecskehát 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. [2] [3]
Indeterminate sauropod remains once misattributed to the Cetiosauridae are present in the province of Kecskemét, Hungary.[ citation needed]
Dinosaurs of the Kecskehát 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] |
Color key
|
Notes Uncertain or tentative taxa are in small text; |
Kecskehát Limestone | |
---|---|
Stratigraphic range:
Pliensbachian ~ | |
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 | Kecskehát 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. [2] [3]
Indeterminate sauropod remains once misattributed to the Cetiosauridae are present in the province of Kecskemét, Hungary.[ citation needed]
Dinosaurs of the Kecskehát 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] |
Color key
|
Notes Uncertain or tentative taxa are in small text; |