Wetterstein Formation
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 (Wetterstein Limestone), Wettersteindolomit ("Wetterstein Dolomite") and combinations thereof. The Wetterstein Formation reaches a maximum thickness of 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. 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: The Swiss stratigraphical lexicon uses Wetterstein Formation as "informal, but used name" with the following historical variants: Subunits. Its subunits include: Description. The Wetterstein Formation, with a total thickness of up to , 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 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. 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. 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. 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. 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. 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. 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: