Schrattenkalk Formation

Last updated
Schrattenkalk Formation
Stratigraphic range: Barremian-Aptian
Schrattenkalk.JPG
Schrattenkalk in Luzern, Switzerland
Type Geological formation
Sub-unitsLower Schrattenkalk, Rawil Member, Upper Schrattenkalk
Underlies Garschella Formation
Overlies Tierwis Formation
Thicknessup to 300 m (980 ft)
Lithology
Primary Limestone
Other Sandstone, mudstone
Location
Coordinates 46°58′30″N8°19′49″E / 46.9751°N 8.3303°E / 46.9751; 8.3303
Approximate paleocoordinates 31°36′N18°30′E / 31.6°N 18.5°E / 31.6; 18.5
Region Alps
CountryFlag of Austria.svg  Austria
Flag of Germany.svg  Germany
Flag of Switzerland (Pantone).svg  Switzerland
Type section
Named for Schrattenfluh
Named by Bernhard Studer
Year defined1834
Switzerland relief location map.jpg
Green pog.svg
Schrattenkalk Formation (Switzerland)

The Schrattenkalk Formation is a Barremian to Aptian geologic formation in the Alps. The limestone is highly karstified. Fossil ornithopod tracks have been reported from the formation. [1] Iguanodont tracks have been registered in the Swiss portion of the formation. [2] The famous north face of the Eiger is partly composed of Schrattenkalk, [3] as well as the Sturmannshöhle in southernmost Bavaria, Germany, [4] and the Hölloch (second-longest cave in Europe) and Silberen system karst caves in Switzerland. [5]

Contents

Description

The formation is named after the Schrattenfluh in Luzern, Switzerland. The name is derived from the Swiss-German "Schratten" (a synonym of Karren) meaning clints or lapies, a phenomenon that frequently affects the limestone. [6] Kalk is limestone in German. Synonyms for the extensive formation are Hieroglyphenkalk, Calcaire à Hippurites, Urgonien, Rudistenkalk, Urgo-Aptien, Schrattenschichten, Requienenkalk, Rhodanien, Caprotinenkalk, and Urgonian Limestone. [7] The formation consists of three units, the Lower Schrattenkalk, Rawil Member and Upper Schrattenkalk.

The upper and lower units consist mostly of reefal limestones with bryozoa, gastropods, corals, sponges, brachiopods, bivalves and rudists. The Rawil Member contains beds of sandstones and mudstones containing foraminifera and echinoderms. The upper and lower members represent a photozoan-dominated carbonate platform, [8] and was deposited at the northern edge of the Tethys Ocean. [9]

Fossil content

In 2015, two new corals were described from Austria; Cairnsipsammia , [10] and Paraclausastrea vorarlbergensis . [11]

In an abandoned quarry on the shore of Lake Lucerne, close to the village of Beckenried, fossil trackways were discovered in the formation. The steeply inclined surface has more than 50 tracks (in three trackways) of ornithopod dinosaurs that are attributed to iguanodontids. Three trackways can be followed for distances of 25 to 35 metres (82 to 115 ft). The lengths of the footprints have a mean of 30 centimetres (12 in) and point to animals ranging in size of 4 to 6 metres (13 to 20 ft), with estimated hip heights between 1.8 and 2 metres (5.9 and 6.6 ft) and 1.4 to 1.7 metres (4.6 to 5.6 ft). [12]

Panorama

Hengst Westpanorama.jpg
Panorama of the Schrattenkalk at the Schrattenfluh

See also

Related Research Articles

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References

  1. Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
  2. Risleten Quarry tracksite at Fossilworks.org
  3. Toni P. Labhart: Geologie der Schweiz. 5., überarb. Auflage. Ott Verlag, Thun 2001, S. 78ff.
  4. Ulrich Lagally, Stefan Glaser, Elisabeth Jobe, Georg Loth, Andreas Murr, Hubert Schmid, Wolfgang Schmid, Klaus Schwerd, Stephan Sieblitz und Ulrich Teipel: Geotope in Schwaben. In: Bayerisches Landesamt für Umwelt (Hrsg.): Erdwissenschaftliche Beiträge zum Naturschutz. Band 7. Augsburg 2009, ISBN   978-3-936385-34-2, S. 132.
  5. Jeannin, 2016, p.49
  6. Bonvallet, 2015, p.14
  7. Bodin, 2006, p.11
  8. Bodin, 2006, p.68
  9. Schrattenkalk Formation at Strati.ch
  10. Rosemarie C. Baron-Szabo (2015). "A new dendrophylliid coral genus Cairnsipsammia from the Lower Cretaceous of western Austria (Anthozoa; Scleractinia; Vorarlberg; Schrattenkalk Formation [upper Barremian-lower Aptian])". Proceedings of the Biological Society of Washington. 128 (4): 216–226. doi:10.2988/0006-324X-128.4.216. S2CID   85709658.
  11. Rosemarie C. Baron-Szabo (2015). "Paraclausastrea vorarlbergensis sp. nov.; a new coral from the Lower Cretaceous of western Austria (Scleractinia; upper Barremian-lower Aptian; Schrattenkalk Fm.; Vorarlberg)". Zootaxa. 4032 (3): 327–332. doi:10.11646/zootaxa.4032.3.9. PMID   26624368.
  12. Meyer, Christian; Thuring, Basil (2003). "The First Iguanodontid Dinosaur Tracks from the Swiss Alps (Schrattenkalk Formation, Aptian)" (PDF). Ichnos. 10 (2–4): 221–228. doi:10.1080/10420940390256186. S2CID   129688898.

Bibliography

Further reading