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Süntel Formation

Geological formation in Germany From Wikipedia, the free encyclopedia

Süntel Formationmap
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The Süntel Formation, previously known as the Kimmeridge Formation (German: "Mittlerer Kimmeridge"; Middle Kimmeridge),[1] is a geological formation in Germany. It is Late Jurassic in age, spanning the early to late Kimmeridgian stage. It predominantly consists of limestone deposited in shallow marine carbonate ramp conditions.[2]

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Description

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Map of the Lower Saxon Hills with Süntel center-right

The formation is part of the Lower Saxony Basin that borders the Süntel massif of the Lower Saxon Hills, part of the larger Harz Mountains. The formation is described as alternations of glauconitic marl, limestone and sandstone.[3]

Paleontological significance

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The formation is known for its fossils, with the Langenberg Quarry having provided fossils of numerous vertebrates.

Dinosaurs

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Turtles

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Squamates

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Pterosaurs

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Crocodyliformes

More information Crocodyliformes of the Süntel Formation, Genus ...

Mammaliaforms

More information Mammaliaforms of the Süntel Formation, Genus ...

Ichnofossils

More information Ichnofossils of the Süntel Formation, Genus ...
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See also

References

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