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
Color key
Notes Uncertain or tentative taxa are in small text ; crossed out taxa are discredited.
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 .
Reptiles
Synapsids
Amphibians
Bony fish
Cartilaginous fish
References
^ "Erfurt Formation" . BGR. Archived from the original on 10 February 2013. Retrieved 2 March 2013 .
^ Erfurt Formation at Fossilworks .org
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^ Rieppel, Olivier (1994). Osteology of Simosaurus gaillardoti and the relationships of stem-group Sauropterygia . [Chicago, Ill.]: Field Museum of Natural History.
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^ Maisch, Michael W. (2009-01-01). "No dicynodont in the Keuper - a reconsideration of the occurrence of aff. Dinodontosaurus in the Middle Triassic of Southern Germany" . Palaeodiversity . 2 : 271–278.
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^ R., Schoch, Rainer (1999). Comparative osteology of Mastodonsaurus giganteus (Jaeger, 1828) from the Middle Triassic (Lettenkeuper: Longobardian) of Germany (Baden-Württemberg, Bayern, Thüringen) . Staatl. Museum für Naturkunde. OCLC 247114091 . {{cite book }}
: CS1 maint: multiple names: authors list (link )
^ Schoch, Rainer R.; Milner, Andrew R.; Witzmann, Florian (September 2014). Ruta, Marcello (ed.). "Skull morphology and phylogenetic relationships of a new Middle Triassic plagiosaurid temnospondyl from Germany, and the evolution of plagiosaurid eyes" . Palaeontology . 57 (5): 1045–1058. Bibcode :2014Palgy..57.1045S . doi :10.1111/pala.12101 . S2CID 130014545 .
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^ Romano, C.; Kogan, I.; Jenks, J.; Jerjen, I.; Brinkmann, W. (2012-09-28). "Saurichthys and other fossil fishes from the late Smithian (Early Triassic) of Bear Lake County (Idaho, USA), with a discussion of saurichthyid palaeogeography and evolution" . Bulletin of Geosciences : 543–570. doi :10.3140/bull.geosci.1337 . ISSN 1802-8225 .