The Travenanzes Formation is a Late Triassic (early Carnian, or early Tuvalian in the regional stratigraphy) limestone, marl and dolomite formation in the Southern Limestone Alps in Trentino-Alto Adige, Italy.
Description
The Travenanzes Formation is conformably overlain by the Dolomia Principale, and overlies the Heiligkreuz Formation separated by an unconformity. Deposition of the formation took place just after the Carnian Pluvial Event (CPE).
Fossil content The following fossils have been described from the Travenanzes Formation:
Ichnofossils
See also
References
Bibliography Bernardi, M.; Gianolla, P.; Petti, F.M.; Mietto, P.; Benton, M. J. (2018), "Dinosaur diversification linked with the Carnian Pluvial Episode", Nature Communications, 9 (1): 1–10, Bibcode:2018NatCo...9.1499B, doi:10.1038/s41467-018-03996-1, PMC 5902586, PMID 29662063 Text and images are available under a Creative Commons Attribution 4.0 International License Bernardi, M.; Petti, F. M.; Avanzini, M. (2010), "A webbed archosaur footprint from the Upper Triassic (Carnian) of the Italian southern Alps. In J. Milàn, S. G. Lucas, M. G. Lockley, & J. A. Spielmann (eds.), Crocodyle Tracks and Traces", New Mexico Museum of Natural History and Science Bulletin, 51: 65–68 D'Orazi Porchetti, S.; Nicosia, U.; Mietto, P.; Petti, F. M.; Avanzini, M. (2008), "Atreipus-like footprints and their co-occurrence with Evazoum from the upper Carnian (Tuvalian) of Trentino-Alto Adige", Studi Trentini di Scienze Naturali, Acta Geologica, 83: 277–287

