To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Schlern Formation

From Wikipedia, the free encyclopedia

Schlern Formation
Stratigraphic range: late Anisian-mid Ladinian
~242–239 Ma
TypeGeologic formation
UnderliesCassian Dolomite
OverliesContrin Formation
Lithology
PrimaryDolomite
OtherLimestone, marl
Location
Coordinates46°36′N 13°18′E / 46.6°N 13.3°E / 46.6; 13.3
Approximate paleocoordinates6°48′N 23°30′E / 6.8°N 23.5°E / 6.8; 23.5
RegionKärnten
South Tyrol
Country Austria
 Italy
ExtentSouthern Limestone Alps
Schlern Formation (Austria)

The Schlern Formation, also known as Schlern Dolomite, and Sciliar Formation or Sciliar Dolomite in Italy, is a limestone, marl and dolomite formation in the Southern Limestone Alps in Kärnten, Austria and South Tyrol, Italy.[1][2][3]

Description

Stratigraphy of the Dolomites

It preserves fossils dating back to the Middle Triassic period (late Anisian-middle Ladinian), or Illyrian to Longobardian in the regional stratigraphy. The formation correlates with the Wetterstein Formation of the Northern Limestone Alps. The formation is also coeval with the Livinallongo or Buchenstein Formation. The Schlern Formation is unconformably overlain by the Cassian Dolomite, and overlies the Contrin Formation separated by another unconformity. Deposition of the formation took place between the Pelsonian Humid Interval and the Ladinian Humid Interval, that preceded the better known Carnian Pluvial Event (CPE).[4]

In Italy, the unit is recognized in the Civetta and Latemar reef buildups,[2][3] and in Austria at the Gartnerkofel.[1]

Fossil content

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

Bivalves
Gastropods

See also

References

  1. ^ a b Schlern Formation at Fossilworks.org
  2. ^ a b Schlern 1 Formation at Fossilworks.org
  3. ^ a b Sciliar Dolomite at Fossilworks.org
  4. ^ Bernardi et al., 2018, p.3
  5. ^ Ogilvie Gordon, 1927
  6. ^ a b c d e f g h i j Friesenbichler et al., 2019
  7. ^ a b c Böhm, 1895

Bibliography

  • Friesenbichler, E.; M. Hautmann; A. Nützel; M. Urlichs, and H. Bucher. 2019. Palaeoecology of Late Ladinian (Middle Triassic) benthic faunas from the Schlern/Sciliar and Seiser Alm/Alpe di Siusi area (South Tyrol, Italy). Paläontologische Zeitschrift 93. 1–29. .
  • Bernardi, M.; P. Gianolla; F.M. Petti; P. Mietto, and M. J. Benton. 2018. Dinosaur diversification linked with the Carnian Pluvial Episode. Nature Communications 9. 1–10. . doi:10.1038/s41467-018-03996-1
    Text and images are available under a Creative Commons Attribution 4.0 International License
  • Ogilvie Gordon, M. M.. 1927. Das Grödener-, Fassa- und Enneberggebiet in den Südtiroler Dolomiten: Geologische Beschreibung mit besonderer Berücksichtigung der Überschiebungserscheinungen. Teil III. Paläontologie. Abhandlungen der Geologischen Bundesanstalt 24. 1–88. .
  • Böhm, J. 1895. Die Gastropoden des Marmolatakalkes. Palaeontographica 42. 211–308. .

Further reading

  • A. Emmerich, V. Zamparelli, T. Bechstädt and R. Zühlke. 2005. The reefal margin and slope of a Middle Triassic carbonate platform: the Latemar (Dolomites, Italy). Facies 50(3-4):573-614
  • J. Pfeiffer. 1988. Paleontology and microfacies of a platform margin in the Carnic Alps (Austria, Middle Triassic). Facies 19:33-60
  • E. Fois and M. Gaetani. 1981. The northern margin of the Civetta buildup. Evolution during the Ladinian and the Carnian. Rivista Italiana di Paleontologia e stratigrafia 86(3):469-542
  • E. Fois. 1981. The Sass da Putia carbonate buildup (western Dolomites): biofacies succession and marginal development during the Ladinian. Rivista Italiana di Paleontologia e Stratigrafia 87(4):565-598
This page was last edited on 29 December 2023, at 23:39
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.