Stratigraphy and facies of an oligocene fringing reef (Castro Limestone,Salento Peninsula,Southern Italy) |
| |
Authors: | Dr Francesca R Bosellini Prof Dr Antonio Russo |
| |
Institution: | (1) Istituto di Paleontologia, Università di Modena, via Università 4, I-41100 Modena |
| |
Abstract: | Summary The coastline of the Salento Peninsula (Apulia region, Southern Italy) is characterized by a rocky shore with spectacular
cliffs where the investigated fringing reef complex, the so called Castro Limestone, spectacularly outcrops for at least 40
km.
As reconstructed from several measured sections, the Castro Limestone, which is Middle Chattian in age from our own data,
disconformably mantles a tectonically deformed falaise of Cretaceous-Eocene rocks and is overlain by a remarkable erosional
surface characterized by a very peculiar rhodolite rudstone. The Castro Limestone unit can be considered as a classic unconformity
bounded depositional sequence representing, most probably, a shelf margin prograding complex, related to the major Middle
Oligocene sea level lowstand.
Stratigraphic and sedimentologic features, together with paleontological characters, allow recognition of a virtually complete
range of reef environments across the reef profile.
Several geomorphic zones and associated facies are described, from the most landward reef area (‘back reef’) across the reef
flat and reef from downward to the fore reef slope, contributing to a better knowledge of the evolution of Oligocene reefs
and reef communities in Italy and in the Mediterranean area. |
| |
Keywords: | Stratigraphy Facies Model Fringing Reef Corals Castro Limestone Salento Peninsula (Southern Italy) Oligocene (Chattian) |
本文献已被 SpringerLink 等数据库收录! |
|