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Erfurt Formation

Coordinates: 50°56′57″N 11°04′12″E / 50.949036°N 11.070136°E / 50.949036; 11.070136
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This is an old revision of this page, as edited by 125.253.47.206 (talk) at 09:58, 1 May 2017 (Fossils: Changed references to dinosaurs being found in the Erfurt to archosauriforms, as no dinosaurian remains are known from any formation of this age). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Erfurt Formation

Stratigraphic range: Ladinian
TypeGeological formation
Unit ofLower Keuper
UnderliesGrabfeld Formation
OverliesUpper Muschelkalk
Thickness20 to 700 m.[1]
Location
Coordinates50°56′57″N 11°04′12″E / 50.949036°N 11.070136°E / 50.949036; 11.070136
RegionMittelgebirge, North German Plain
CountryGermany
Type section
Named forErfurt
Named byHoffmann, 1830
Lithostratigraphy of the Keuper of the Germanic basin.

The Erfurt Formation is a stratigraphic formation of the Keuper group and the Germanic Trias supergroup. It was deposited during the Ladinian. It lies above the Upper Muschelkalk and below the Middle Keuper.[1]

Definition

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

The Erfurt Formation is underlain by the Upper Muschelkalk. 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 Grabfeld Formation.[1]

Fossils

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.[2]

References

  1. ^ a b c d e "Erfurt Formation". BGR. Archived from the original on 10 February 2013. Retrieved 2 March 2013. {{cite web}}: Unknown parameter |dead-url= ignored (|url-status= suggested) (help)
  2. ^ 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.