The Gerola Valley site (Orobic Basin, Northern Italy): A key for understanding late Early Permian tetrapod ichnofaunas
Articolo
Data di Pubblicazione:
2015
Abstract:
A taxonomic study has been carried out on the historical Gerola Valley locality (Pizzo del Diavolo formation, late
Cisuralian), which represents one of the best tetrapod ichnosites of the whole Southern Alps (North Italy). With
respect to previous studies, the ichnoassociation is now enlarged and lists the following taxa: Amphisauropus,
Dromopus, Erpetopus, Hyloidichnus, Limnopus, Varanopus. The optimal preservation of the material, which in
some cases shows even traces of the skin, allowed the recognition of a new morphotype of Varanopus. The invertebrate ichnoassociation is newly described and is representative of impoverished Scoyenia and Mermia
ichnofacies. A detailed facies analysis of the uppermost arenitic–pelitic lithofacies of the Pizzo del Diavolo
formation, which revealed the most abundant fossil content (Locality 1) and of two new localities (pelitic facies,
Localities 2, 3) shows a transition from shallow lacustrine to floodplain and alluvial fan environments under a
generally dry climate. Besides the taxonomic revision of vertebrate tracks, the final aims of our study are:
i) the depositional, palaeoenvironmental and climatic reconstruction of this sector of the Orobic Basin through
an integration of palaeontological data and facies analysis; and ii) the regional correlation of this key stratigraphic
succession with other coeval ichnofaunas in Pangaea.
Cisuralian), which represents one of the best tetrapod ichnosites of the whole Southern Alps (North Italy). With
respect to previous studies, the ichnoassociation is now enlarged and lists the following taxa: Amphisauropus,
Dromopus, Erpetopus, Hyloidichnus, Limnopus, Varanopus. The optimal preservation of the material, which in
some cases shows even traces of the skin, allowed the recognition of a new morphotype of Varanopus. The invertebrate ichnoassociation is newly described and is representative of impoverished Scoyenia and Mermia
ichnofacies. A detailed facies analysis of the uppermost arenitic–pelitic lithofacies of the Pizzo del Diavolo
formation, which revealed the most abundant fossil content (Locality 1) and of two new localities (pelitic facies,
Localities 2, 3) shows a transition from shallow lacustrine to floodplain and alluvial fan environments under a
generally dry climate. Besides the taxonomic revision of vertebrate tracks, the final aims of our study are:
i) the depositional, palaeoenvironmental and climatic reconstruction of this sector of the Orobic Basin through
an integration of palaeontological data and facies analysis; and ii) the regional correlation of this key stratigraphic
succession with other coeval ichnofaunas in Pangaea.
Tipologia CRIS:
1.1 Articolo in rivista
Keywords:
Tetrapod footprints
Invertebrate trace fossils
Fluvio-lacustrine succession
Freshwater carbonates
Pizzo del Diavolo formation
Elenco autori:
Marchetti, L.; Ronchi, A.; Santi, Giuseppe; Voigt, S.
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