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// Workers AI · dad joke modeWhat did the Gosau Group say? "We're a rock solid team

Gosau Group
Stratigraphic range: Late Cretaceous-Eocene
~90–50 Ma
Rocks of the Gosau Group exposed in the Imster Muttekopf
Typestratigraphic group
Sub-units
OverliesUnconformity with folded and faulted Permian to Lower Cretaceous rocks
Thickness2,200–2,600 m (7,200–8,500 ft)
Location
Coordinates47°36′N 13°30′E / 47.6°N 13.5°E / 47.6; 13.5
Approximate paleocoordinates32°06′N 15°36′E / 32.1°N 15.6°E / 32.1; 15.6
RegionCentral Europe
CountryAustria
Germany
Slovakia
ExtentGosau Basin, Limestone Alps
Gosau Group is located in Austria
Gosau Group
Gosau Group
Gosau Group
Gosau Group
Gosau Group
Gosau Group
Gosau Group
Gosau Group
Gosau Group (Austria)

The Gosau Group (German: Gosau-Gruppe) is a lithostratigraphic term for a geological unit found in Austria, Germany, western Slovakia and Romania. The sediments were deposited between the Late Cretaceous to Eocene[1] and are exposed in numerous isolated basins within the Northern Calcareous Alps. The group is divided into two subgroups, the Lower Gosau Subgroup which dates from the Turonian to Campanian, approximately 90 to 75 Ma and the Upper Gosau Subgroup which dates to the Santonian to Eocene, about 83.5 to 50 Ma.[2]

In the Gosau Basin the unit is over 2,300 m (7,500 ft) thick. The formations within each subunit vary significantly between basin. The sequence is largely marine, but the Grünbach Formation represents a terrestrial deposit and to the south-west of Vienna coal deposits have been worked in the Gosau.[3](p21) There are many fossiliferous units in the group, these contain both marine fossils such as ammonites and terrestrial remains, including those of dinosaurs, in the Grünbach Formation and Schönleiten Formation.

Stratigraphic contacts between the Gosau beds and any earlier units are generally unconformable and the isolated pockets in which they occur are often fault bounded.[3](p21) Because the Gosau Group is a lithostratigraphic unit the time of deposition (in Ma before present) may be vary from place to place but the younger Gosau beds can be distinguished from those which are older than lower Campanian by the assemblage of 'heavy minerals' they contain and in some basins the fossil content allows more accurate dating.[4]

Tectonic relevance

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Upper Cretaceous sediments, particularly the Gosau beds, have been of importance in interpreting the tectonic history of the Northern Calcareous Alps.[3](p19 & 21)

Gosau beds rest unconformably on thrust contacts between sheets in the Northern Calcareous Alps. The unconformable relationship indicates that the early stages of thrusting ('pre-Gosau') had commenced before the Gosau units were deposited in the upper Cretaceous. During later 'post-Gosau' movements the Gosau beds were severely faulted. Those later events involved flexure folding and the northward movement of the Northern Calcareous Alps resulting in it overlying areas of the molasse deposits of Miocene age.[5]

Fossil content

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Fossils which have been described from the Gosau Group include:[6][7]

reptiles
GenusSpeciesPresenceNotesImages
Struthiosaurus S. austriacus Niederösterreich, Austria [8]
Mochlodon M. suessi A rhabdodontid iguanodont[8]
Rhadinosaurus R. alcinus Possible indeterminate ankylosaur remains[8]
"Crataeomus" C. lepidophorus Later found to be synonymous with Struthiosaurus austriacus[8]
C. pawlowitschii Later found to be synonymous with Struthiosaurus austriacus in partim[8]
"Danubiosaurus" D. anceps Later found to be indeterminate ankylosaurian and Struthiosaurus austriacus remains in partim[8]
"Indeterminate fragments"[9]
"Hoplosaurus" H. ischyrus Later found to be synonymous with Struthiosaurus austriacus[8]
"Leipsanosaurus" L. noricus Later found to be synonymous with Struthiosaurus austriacus[8]
"Pleuropeltus" P. suessi Later found to be synonymous with Struthiosaurus austriacus in partim[8]
"Megalosaurus" M. pannoniensis Later found to be indeterminate theropod remains[8]
Ornithocheiridae indet. [10][11]
Mollusca
GenusSpeciesPresenceNotesImages
"Trochactaeon" T. conicus Nördliche Kalkalpen, Niederösterreich, Austria Very common fossil, rock forming
Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

See also

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References

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  1. Höfling, 1985
  2. McCann, T (2008). The Geology of Central Europe- Volume 2 Mesozoic and Cenozoic. Geological Society of London. pp. 975–978. ISBN 978-1862392656.
  3. 1 2 3 Oxburgh, E.R. (1968). The Geology of the Eastern Alps. The Geologists Association. ISBN 978-0-913312-33-9. Retrieved 22 July 2025.
  4. Stattegger, Karl (1987). "Heavy minerals and provenance of sands; modeling of lithological end members from river sands of northern Austria and from sandstones of the Austroalpine Gosau Formation (Late Cretaceous)". Journal of Sedimentary Research. 57 (2): 301–310. doi:10.1306/212F8B0C-2B24-11D7-8648000102C1865D. Retrieved 7 August 2025.
  5. Linzer, Hans-Gert; Ratschbacher, Lothar; Frisch, Wolfgang (1995). "Transpressional collision structures in the upper crust: the fold-thrust belt of the Northern Calcareous Alps". Tectonophysics. 242 (1–2): 41–61. Bibcode:1995Tectp.242...41L. doi:10.1016/0040-1951(94)00152-Y. Retrieved 5 August 2025.
  6. Gosau Group at Fossilworks.org
  7. Lower Gosau Group at Fossilworks.org
  8. 1 2 3 4 5 6 7 8 9 10 Weishampel, 2004, pp. 588-593
  9. "Table 17.1," in Weishampel et al., 2004, p.367
  10. Zitteliana
  11. Agnolin & Varricchio, 2012

Bibliography

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Further reading

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