Erfurt Formation

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. It lies above the Upper Muschelkalk and below the Middle Keuper.
Definition.
The formation was defined in Erfurt-Melchendorf in 1830 by Franz Xaver Hofmann and named for the nearby town of Erfurt.
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.
The upper boundary is marked by dolomites, or claystones of the Grabfeld Formation.
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".