Erfurt Formation

Erfurt Formation
Stratigraphic range: Ladinian
~242–237 Ma

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Erfurt Formation; Stratigraphic range: Ladinian; ~242–237 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓
	Outcrop of the formation in Vellberg
Type	Geological formation
Unit of	Lower Keuper
Sub-units	Bairdienkalk, Grenzdolomit, Lettenkeuper, Sandige Pflanzenschiefer, Untere Graue Mergel & Werksandstein Members
Underlies
Overlies	Upper Muschelkalk
Thickness	20–700 m (66–2,297 ft)
Lithology
Primary	Marl
Other	Claystone, dolomite, limestone, sandstone
Location
Coordinates	50°56′57″N 11°04′12″E / 50.949036°N 11.070136°ECoordinates: 50°56′57″N 11°04′12″E / 50.949036°N 11.070136°E
Approximate paleocoordinates	15°06′N 16°36′E / 15.1°N 16.6°E
Region	Baden-Württemberg, Thuringia
Country	Germany
Extent	Mittelgebirge, North German Plain
Type section
Named for	Erfurt
Named by
Year defined	1830
	Erfurt Formation (Germany)

Lithostratigraphy of the Keuper of the

The Erfurt Formation, also known as the Lower Keuper (German: Untere Keuper, Lettenkeuper, Lettenkohle or Lettenkohlenkeuper), is a stratigraphic formation of the Keuper group and the Germanic Trias supergroup. It was deposited during the Ladinian stage of the Triassic period.^[2] It lies above the and below the .^[1]

Definition[]

The formation was defined in Erfurt-Melchendorf in 1830 by and named for the nearby town of Erfurt.^[1]

The Erfurt Formation is underlain by the . The lower boundary to the Erfurt Formation is the "Lettenkohlensandstein" in northern Germany and the "Grenz-bone-beds" in southern Germany.

The formation is a sequence of dolomite, lacustrine limestones, claystone, evaporites, and fluviatile sandstones. The color is usually grey but can also be brown or reddish brown. The average thickness is 60 to 80 meter, with a maximum thickness of 700 meter in the Glückstadt-Graben.^[1]

The upper boundary is marked by dolomites, or claystones of the .^[1]

Fossil content[]

The Erfurt Formation is known for its vertebrate fossils. Different kinds of fish, amphibians and archosauriforms have been found. Usually they are found as bone beds, but in 1977 the first complete skeletons were found near Kupferzell. They include Mastodonsaurus, Gerrothorax, Plagiosuchus, Callistomordax, Nanogomphodon, Batrachotomus, Kupferzellia and Palaeoxyris friessi.^[3]

References[]

^ ^a ^b ^c ^d ^e "Erfurt Formation". BGR. Archived from the original on 10 February 2013. Retrieved 2 March 2013.
^ Erfurt Formation at Fossilworks.org
^ Ronald Böttcher (2010). "Description of the shark egg capsule Palaeoxyris friessi n. sp. from the Ladinian (Middle Triassic) of SW Germany and discussion of all known egg capsules from the Triassic of the Germanic Basin" (PDF). Palaeodiversity. 3: 123–139. Retrieved 23 January 2012.

[BGR-1] "Erfurt Formation". BGR. Archived from the original on 10 February 2013. Retrieved 2 March 2013.

[FW-2] Erfurt Formation at Fossilworks.org

[3] Ronald Böttcher (2010). "Description of the shark egg capsule Palaeoxyris friessi n. sp. from the Ladinian (Middle Triassic) of SW Germany and discussion of all known egg capsules from the Triassic of the Germanic Basin" (PDF). Palaeodiversity. 3: 123–139. Retrieved 23 January 2012.

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