The finding of Asteriacites lumbricalis in the Lower Jurassic of the Trento carbon- ate Platform is here integrated with the sedimentological, stratigraphical, and palaeon- tological data for the Coste dell'Anglone ichnosite in order to better reconstruct its palaeoenvironmental setting. The presence of these traces produced by small ophi- uroids support the interpretation, for this geographical sector during the middle-late Sinemurian, of a marginal-marine tidal flat environment. A marginal marine environ- ment is consistent also with the documented existence of sedentary populations of dinosaurs recorded as footprints in the deposits that overlie those preserving Asteria- cites.

Bernardi, M.; Petti, F.M.; Avanzini, M. (2010). Palaeoenvironmental implications of Asteriacites lumbricalis in the Coste dell'Anglone dinosaur ichnosite (NE Italy).: 1-8.

Palaeoenvironmental implications of Asteriacites lumbricalis in the Coste dell'Anglone dinosaur ichnosite (NE Italy)

BERNARDI, MASSIMO;AVANZINI, MARCO
2010-01-01

Abstract

The finding of Asteriacites lumbricalis in the Lower Jurassic of the Trento carbon- ate Platform is here integrated with the sedimentological, stratigraphical, and palaeon- tological data for the Coste dell'Anglone ichnosite in order to better reconstruct its palaeoenvironmental setting. The presence of these traces produced by small ophi- uroids support the interpretation, for this geographical sector during the middle-late Sinemurian, of a marginal-marine tidal flat environment. A marginal marine environ- ment is consistent also with the documented existence of sedentary populations of dinosaurs recorded as footprints in the deposits that overlie those preserving Asteria- cites.
Geologia
articolo in rivista
2010
pubblicato
1
8
No
con Impact Factor
si
Bernardi, M.; Petti, F.M.; Avanzini, M.
Bernardi, M.; Petti, F.M.; Avanzini, M. (2010). Palaeoenvironmental implications of Asteriacites lumbricalis in the Coste dell'Anglone dinosaur ichnosite (NE Italy).: 1-8.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/10991/401
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