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Link to original content: http://en.wikipedia.org/wiki/Werfen_Formation
Werfen Formation - Wikipedia Jump to content

Werfen Formation

Coordinates: 46°48′N 12°06′E / 46.8°N 12.1°E / 46.8; 12.1
From Wikipedia, the free encyclopedia
Werfen Formation
Stratigraphic range: Changhsingian-Ladinian
~254–235 Ma
TypeFormation
Unit ofCostabella Group
Sub-unitsCampil, Cencenighe, Gastropod Oolite, Tesero Oolite, Mazzin, Siusi, Val Badia Members
Lithology
PrimaryMudstone, lime mudstone, limestone
OtherSiltstone, sandstone, marl
Location
Coordinates46°48′N 12°06′E / 46.8°N 12.1°E / 46.8; 12.1
Approximate paleocoordinates7°24′N 22°54′E / 7.4°N 22.9°E / 7.4; 22.9
RegionUpper Austria,
Bolzano, South Tyrol, Trentino, Veneto
CountryAustria
Italy
Bosnia and Herzegovina
ExtentDinaric, Southern Limestone & Salzburg Slate Alps, Tennen Mountains
Type section
Named forWerfen
Werfen Formation is located in Mediterranean
Werfen Formation
Werfen Formation
Werfen Formation (Mediterranean)

The Werfen Formation is a geologic formation in the Southern Limestone Alps and Dinaric Alps of Austria, Bosnia and Herzegovina, and Italy. It preserves fossils dating back to the Triassic period.[1]

Fossil content

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The formation has provided numerous fossils typical of a shallow lagoon environment, including:

Griesbachian aged layers of the formation also preserve an unexpectedly diverse ichnotaxon assemblage, including the ichnogenera Catenichnus, Helminthopsis, Lockeia, Palaeophycus, Planolites, Rhizocorallium, Spongeliomorpha, Taenidium and Thalassinoides.[3]

See also

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References

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  1. ^ Werfen Formation at Fossilworks.org
  2. ^ a b c Thompson, Jeffrey R.; Posenato, Renato; Bottjer, David J.; Petsios, Elizabeth (2019). "Echinoids from the Tesero Member (Werfen Formation) of the Dolomites (Italy): implications for extinction and survival of echinoids in the aftermath of the end-Permian mass extinction". PeerJ. 7: e7361. doi:10.7717/peerj.7361. PMC 6718154. PMID 31531267.
  3. ^ Hofmann, Richard; Goudemand, Nicolas; Wasmer, Martin; Bucher, Hugo; Hautmann, Michael (2011). "New trace fossil evidence for an early recovery signal in the aftermath of the end-Permian mass extinction". Palaeogeography, Palaeoclimatology, Palaeoecology. 310 (3–4): 216–226. Bibcode:2011PPP...310..216H. doi:10.1016/j.palaeo.2011.07.014.

Bibliography

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Further reading

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  • E. Farabegoli, M. C. Perri, and R. Posenato. 2007. Environmental and biotic changes across the Permian-Triassic boundary in western Tethys: The Bulla parastratotype, Italy. Global and Planetary Change 55:109-135
  • E. Kustatscher, M. Wachtler, and J.H.A. Konijnenburg-van Cittert. 2004. A number of additional and revised taxa from the Ladinian flora of the Dolomites, Northern Italy. Geo.Alp 1:57-69
  • R. Posenato. 2009. Survival patterns of macrobenthic marine assemblages during the end-Permian mass extinction in the western Tethys (Dolomites, Italy). Palaeogeography, Palaeoclimatology, Palaeoecology 280:150-167
  • A. Bittner. 1890. Brachiopoden der alpinen Trias. Abhandlungen der Kaiserlich-Königlichen Geologischen Reichsanstalt 14:1-325