Allgäu Formation

Allgäu Formation Stratigraphic range: Hettangian-Sinemurian (-) ~201–191 Ma PreꞒ Ꞓ O S D C P T J K Pg N
Type	Formation
Sub-units	Alpisella beds
Lithology
Primary	Marl
Other	Limestone
Location
Coordinates	47°42′N 13°42′E / 47.7°N 13.7°E / 47.7; 13.7Coordinates: 47°42′N 13°42′E / 47.7°N 13.7°E / 47.7; 13.7
Approximate paleocoordinates	32°30′N 19°54′E / 32.5°N 19.9°E / 32.5; 19.9
Region	Vorarlberg Bavaria Graubünden
Country	Austria  Germany   Switzerland
Allgäu Formation (Austria)

The Allgäu Formation is a geologic formation in Austria. It preserves fossils dating back to the Hettangian to Sinemurian stages of the Early Jurassic period, or to in the regional stratigraphy. Initially and formally defined by Jacobshagen (1965).^[1] The Allgäu Formation is formerly known as spotted marls (Lias-Fleckenmergel) and spotted marly limestones (Fleckenkalk). The formation is represented by dark-grey bioturbated limestones and marlstone interbeds. It represents basinal hemipelagic facies^[2] common in Alpine Tethys regions of Alps, Carpathians and other mountain ranges. Several horizons of the formation are particularly rich in ammonite fauna.

Fossil content[]

Fish

• Agkistracanthus sp.^[3]

Ammonites^[4]

• Echioceras raricostatoides
• Asteroceras cf. suevicum
• Juraphyllites sp.
• Villania sp.

Rhynchonellata^[5]

See also[]

• List of fossiliferous stratigraphic units in Austria
• List of fossiliferous stratigraphic units in Germany
• List of fossiliferous stratigraphic units in Switzerland

References[]

Bibliography[]

• Gawlick, H.J., Missoni, S., Schlagintweit, F., Suzuki, H., Frisch, W., Krystyn, L., Blau, J. & Lein, R., 2009, Jurassic Tectonostratigraphy of the Austroalpine Domain. Journal of Alpine Geology, 50, p. 1–152
• H. Sulser and H. Furrer. 2008. Dimerelloid rhynchonellide brachiopods in the Lower Jurassic of the Engadine (Canton Graubünden, National Park, Switzerland). Swiss Journal of Geosciences 101:203-222
• J. Blau. 1998. Monographie der Ammoniten des Obersinemuriums (Lotharingium, Lias) der Lienzer Dolomiten (Österreich): Biostratigraphie, Systematik und Paläobiogeographie. Revue de Paléobiologie, Genève 17:177-285
• C. J. Duffin and H. Furrer. 1981. Myriacanthid holocephalan remains from the Rhaetian (Upper Triassic) and Hettangian (Lower Jurassic) of Graubünden (Switzerland). Eclogae Geologicae Helvetiae 74:803-829
• Jacobshagen, V. von, 1965, Die Allgäu-Schichten (Jura-Fleckenmergel) zwischen Wettersteingebirge und Rhein. Jb. Geol. B. A., 108, pp. 1–114