The Travenanzes Formation is a
Late Triassic
The Late Triassic is the third and final epoch (geology), epoch of the Triassic geologic time scale, Period in the geologic time scale, spanning the time between annum, Ma and Ma (million years ago). It is preceded by the Middle Triassic Epoch ...
(
early Carnian, or
early Tuvalian in the regional stratigraphy)
limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms wh ...
,
marl and
dolomite formation
Formation may refer to:
Linguistics
* Back-formation, the process of creating a new lexeme by removing or affixes
* Word formation, the creation of a new word by adding affixes
Mathematics and science
* Cave formation or speleothem, a secondary ...
in the
Southern Limestone Alps
The Southern Limestone Alps ( it, Alpi Sud-orientali, german: Südliche Kalkalpen), also called the Southern Calcareous Alps, are the ranges of the Eastern Alps south of the Central Eastern Alps mainly located in northern Italy and the adjacent ...
in
Trentino-Alto Adige, Italy.
[Travenanzes Formation]
at Fossilworks
Fossilworks is a portal which provides query, download, and analysis tools to facilitate access to the Paleobiology Database, a large relational database assembled by hundreds of paleontologists from around the world.
History
Fossilworks was cre ...
.org
Description
The Travenanzes Formation is conformably overlain by the
Dolomia Principale
Main Dolomite (german: Hauptdolomit, hu, Fődolomit, it, Dolomia Principale) is a lithostratigraphic unit in the Alps of Europe. Formation was defined by K.W. Gümbel in 1857.
Middle to Late Triassic sedimentary record in the Alpine realm is ...
,
[Bernardi et al., 2018, p.6] and overlies the
Heiligkreuz Formation separated by an unconformity. Deposition of the formation took place just after the
Carnian Pluvial Event
The Carnian pluvial episode (CPE), often called the Carnian pluvial event, was an interval of major change in global climate synchronous with significant changes in Earth's biota both in the sea and on land. It occurred during the latter part of ...
(CPE).
[Bernardi et al., 2018, p.3]
Fossil content
The following fossils have been described from the Travenanzes Formation:
[
;Ichnofossils
* '' Atreipus sp.''][D'Orazi Porchetti et al., 2008]
* '' Evazoum sp.''[
* '' Grallator (Eubrontes)''][
* Crocodylomorpha indet.][Bernardi et al., 2010]
See also
* List of fossiliferous stratigraphic units in Italy
* Montemarcello Formation
* Schlern Formation
* Wetterstein Formation
References
Bibliography
*
Text and images are available under
Creative Commons Attribution 4.0 International License
*
* {{cite LSA , last=D'Orazi Porchetti , first=S. , first2=U. , last2=Nicosia , first3=P. , last3=Mietto , first4=F. M. , last4=Petti , first5=M. , last5=Avanzini , year=2008 , title=''Atreipus''-like footprints and their co-occurrence with ''Evazoum'' from the upper Carnian (Tuvalian) of Trentino-Alto Adige , journal= Studi Trentini di Scienze Naturali, Acta Geologica , volume=83 , pages=277–287
Geologic formations of Italy
Triassic System of Europe
Triassic Italy
Carnian Stage
Dolomite formations
Limestone formations
Marl formations
Reef deposits
Shallow marine deposits
Ichnofossiliferous formations
Paleontology in Italy
Formations
Geology of the Alps