Wetterstein Formation
Stratigraphic range: Ladinian-Carnian
~
The formation in the Wetterstein near Gatterl
TypeGeological formation
Sub-unitsSee text
UnderliesSee text
OverliesSee text
Thicknessup to 1,000 m (3,300 ft)
Lithology
PrimaryLimestone, dolomite
Location
Coordinates45°N 20°W / 45°N 20°W / 45; -20
RegionAlps, Central Europe
Country Austria
 Germany
 Hungary
 Slovakia
ExtentNorthern Limestone Alps, Western Carpathians
Type section
Named forWetterstein Mountains
Named byVon Gümbel
Year defined1861
Coordinates45°N 20°W / 45°N 20°W / 45; -20
Approximate paleocoordinates4°N 4°W / 4°N 4°W / 4; -4
Wetterstein limestone
Stratigraphic range: Middle—Late Triassic
TypeGeological formation
Thickness600 m
Lithology
PrimaryLimestone
Location
RegionAlps, Central Europe
CountryAustria, Germany, Switzerland
Transgression of the Paleogene sediments over the Wetterstein Limestone of the Silicic Superunit, Western Carpathians.

The Wetterstein Formation is a regional geologic formation of the Northern Limestone Alps and Western Carpathians extending from southern Bavaria, Germany in the west, through northern Austria to northern Hungary and western Slovakia in the east. The formation dates back to the Ladinian to Carnian stages of the Late Triassic. The formation is named after the Wetterstein Mountains in southern Germany and northwestern Austria. The center of its distribution, however, is in the Karwendel Mountains. It occurs in the Northern and Southern Limestone Alps and in the Western Carpathians.

The formation is composed of mostly reefal limestones and dolomites, the latter the result of widespread diagenesis. In many areas there is a frequent alternation of limestone and dolomite facies. Local variants to indicate the Wetterstein Formation include German: Wettersteinkalk (Wetterstein Limestone), Wettersteindolomit ("Wetterstein Dolomite") and combinations thereof. The Wetterstein Formation reaches a maximum thickness of 1,000 metres (3,300 ft) with major regional thickness variations. It belongs to the tectonostratigraphical unit Austroalpine nappes. The carbonate rock of the formation is from the Middle Triassic epoch of the Ladinian stage, comparable to the German stage in which Muschelkalk rock strata were formed.

The formation has provided numerous fossils of corals, sponges, bivalves, gastropods and other marine groups indicative of a shallow marine carbonate platform environment deposited at the northern end of the Tethys Ocean.

Naming

Map of the Wetterstein

The Wetterstein Formation is named after the Wetterstein Mountains in southern Germany and northwestern Austria.

Alternative names for the whole formation or parts of it in stratigraphical (vertical) or facies (lateral) sense are:

  • Wetterstein Limestone (Wettersteinkalk)
  • Wettersteinkalk Formation[1]
  • Wettersteindolomit - used in Semmering and Kalkkögel, Austria[2]
  • Wetterstein Limestone Formation[3][4]
  • Wetterstein kalk/dolomit - used in the Northern Limestone Alps of Austria[2]
  • Wetterstein reef limestone Formation[5]
View of the Wetterstein

The Swiss stratigraphical lexicon uses Wetterstein Formation as "informal, but used name" with the following historical variants:[6]

  • Wettersteinkalk (von Guembel 1861, Fraas 1910)
  • Wettersteinkalk = Ladinische Stufe (Cornelius 1935)
  • Wetterstein = Wettersteindolomit = Wettersteinkomplex (Stöcklin 1949) (Fellerer 1964, Kraus 1964)
  • Calcaire de Wetterstein [sic] = Calcaire du Wetterstein = Formation de Wetterstein [sic] (Hirsch 1966)
  • Wettersteindolomit, Wetterstein-Dolomit

Subunits

Its subunits include:

Description

The Wetterstein Formation crops out in the light-grey blue parts of this map, mostly in Austria, with other outcrops in Germany, Hungary and Slovakia

The Wetterstein Formation, with a total thickness of up to 1,000 metres (3,300 ft),[6] is a major regional stratigraphic unit of the Northern Limestone Alps and Western Carpathians in Central Europe, spanning across four countries from southwestern Bavaria to northwestern Slovakia.

Extent

The Tauern Window in the Alps with the Northern Limestone Alps in cyan

The formation crops out to the north of the Hohe Tauern window and is part of the Austroalpine nappes.

Stratigraphy

In the Semmering area of Austria, where the name Wettersteindolomit is used, the formation is unconformably overlain by the Kapellener Shale and overlies the Reifling Formation, in the Kalkkögel and Radstadt Tauern the dolomite overlies the Partnach Formation and is overlain by the Raibl Formation, while in Tyrol the formation, called Wettersteinkalk/dolomit unconformably overlies the Gutenstein and Steinalm Formations and unconformably underlies the Reingraben Formation.[2]

In the Aggtelek-Rudabánya mountains of Hungary, the formation, called Wetterstein Limestone Formation overlies the Reifling and Steinalm Formations and is overlain by the Szádvárborsa Formation.[3]

Regional correlations

In Austria the Wetterstein Dolomite correlates with the Alberg Formation of the Linz Dolomites, the Wetterstein kalk/dolomite with the lower part of the Hallstatt Formation of the Northern Limestone Alps and with the Schlern Dolomite, or Schlern Formation, in the Southern Limestone Alps.[3]

In Hungary, the formation is time-equivalent with the Berva Formation of the Bükk, the Bódvavölgyi Ophiolite, Szentjánoshegy and Derenk Formations of the Aggtelek-Rudabánya range and the Csanádapáca Formation of the Békés Zone.[3] In the Dinarides, the formation is time-equivalent with the Grivska Formation of Bosnia. The Kopaonik Formation in its eponymous mountain range in Serbia is considered a distal, more deep water equivalent of the Wetterstein platform sediments.[7]

Diagenesis

Dolomitization of the Wetterstein Carbonate Platform is a widespread phenomenon, especially in the Tirolic units of the Northern Calcareous Alps. At the Clessinsperre, the type locality for the underlying Steinalm Formation, intense dolomitization has altered the microfacies characteristics of the Wetterstein Carbonate platform – typical are fore-reef carbonates, later reefal and back-reefal carbonates topped by lagoonal carbonates, making the original features hardly visible.[8]

Fossil content

Because, during dolomitisation, traces of fossils are largely lost as a result of recrystallisation, fossils in the Wetterstein dolomite are harder to distinguish, and even in thin sections may be barely recognizable. Wetterstein dolomite is rarely as bituminous as typical Main Dolomite and therefore tends to be much more pure and brighter-coloured. Otherwise, there are no fundamental differences with the Wetterstein limestone.

Among others, the following fossils have been described from the Wetterstein Formation:

GroupUnitFossilsNotes
SpongesWettersteinkalk, AustriaAlpinothalamia bavarica, Follicatena cautica, Colospongia catenulata, Cryptocoelia zitteli, Solenolmia magna, Uvanella irregularis, Vesicocaulis alpinus, V. depressus, V. oenipontanus[9]
Wetterstein reef limestone, HungaryParavesicocaulis concentricus, Senowbaridaryana triassicus, Vesicocaulis multisiphonatus[10]
BrachiopodsWettersteinkalk, AustriaStolzenburgiella baloghi[11]
Corals
Gastropods
Bivalves

See also

References

  1. ↑ Wettersteinkalk Formation at Fossilworks.org
  2. 1 2 3 Piller & Erhart, 2004
  3. 1 2 3 4 Császár, 1997, p.23
  4. ↑ Wetterstein Limestone Formation at Fossilworks.org
  5. ↑ Wetterstein reef limestone Formation at Fossilworks.org
  6. 1 2 Wetterstein Formation at Strati.ch
  7. ↑ Schefer et al., 2010, p.106
  8. ↑ Gawlick et al., 2013, p.182
  9. ↑ Karwendel reef at Fossilworks.org
  10. ↑ Alshóhegy plateau at Fossilworks.org
  11. ↑ Siblik, 1994, p.370

Bibliography

Further reading

  • McCann, Tom. 2008. The Geology of Central Europe: Mesozoic and Cenozoic, 1–736. 2; Geological Society. ISBN 978-1-86239-265-6
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