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Monte Coccovello

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 Monte Coccovello section: lithological–sedimentological log, oxygen- and carbon-isotope stratigraphy, and range of the most significant benthic foraminifers. The section has been subvided into four intervals (A–D) on the basis of lithofacies and biostratigraphy. The δ13C curve has been subdivided into five segments (1–5). The Cenomanian–Turonian boundary is placed according to the most commonly used biostratigraphic schemes (De Castro 1991; Chiocchini et al. 1994).
Published: 01 May 2007
Fig. 2.  Monte Coccovello section: lithological–sedimentological log, oxygen- and carbon-isotope stratigraphy, and range of the most significant benthic foraminifers. The section has been subvided into four intervals (A–D) on the basis of lithofacies and biostratigraphy. The δ 13 C curve has been
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 Schematic geological map of the southern Apennines (modified from Bonardi et al. 1988) with location of studied sections. 1, Monte Coccovello; 2, Monteforte Cilento; 3, Monte Cerreto.
Published: 01 May 2007
Fig. 1.  Schematic geological map of the southern Apennines (modified from Bonardi et al . 1988 ) with location of studied sections. 1, Monte Coccovello; 2, Monteforte Cilento; 3, Monte Cerreto.
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 Comparison with the Eastbourne Chalk curve shows that pre-excursion δ13C values are distinctly lower in the southern Apennine shallow-water sections, even if we consider the envelope of the most positive values on the assumption that it represents values less affected by meteoric diagenesis. Carbon-isotope ratios are more depleted in the section showing the most restricted facies (Monte Coccovello) than in the section where more open-marine conditions are inferred on the basis of facies and fossil associations (Monte Cerreto).
Published: 01 May 2007
diagenesis. Carbon-isotope ratios are more depleted in the section showing the most restricted facies (Monte Coccovello) than in the section where more open-marine conditions are inferred on the basis of facies and fossil associations (Monte Cerreto).
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 Chemostratigraphic correlation of the three studied sections with the standard reference curve of the Eastbourne Chalk, using the nomenclature for the fine structure of the excursion defined by Paul et al. (1999) and the chronostratigraphic calibration of Gale et al. (2005). For easier correlation a scaled and smoothed version of the more expanded Monte Cerreto curve is also shown (see text for further details). Chemostratigraphic correlation allows definition of the age of some shallow-water events to the level of an ammonite zone. The black arrows mark the position of the highest upper Cenomanian emergence surfaces; the grey arrows indicate the first Turonian subaerial exposure surface at Monte Coccovello and the recovery of the shallow-water carbonate factory at Monteforte Cilento.
Published: 01 May 2007
of the highest upper Cenomanian emergence surfaces; the grey arrows indicate the first Turonian subaerial exposure surface at Monte Coccovello and the recovery of the shallow-water carbonate factory at Monteforte Cilento.
Journal Article
Published: 01 May 2007
Journal of the Geological Society (2007) 164 (3): 609–620.
...Fig. 2.  Monte Coccovello section: lithological–sedimentological log, oxygen- and carbon-isotope stratigraphy, and range of the most significant benthic foraminifers. The section has been subvided into four intervals (A–D) on the basis of lithofacies and biostratigraphy. The δ 13 C curve has been...
FIGURES
First thumbnail for: Carbon-isotope stratigraphy of Cenomanian–Turonian...
Second thumbnail for: Carbon-isotope stratigraphy of Cenomanian–Turonian...
Third thumbnail for: Carbon-isotope stratigraphy of Cenomanian–Turonian...
Journal Article
Published: 01 January 2016
Journal of Foraminiferal Research (2016) 46 (1): 9–24.
... Limestone) Formation and the lower part of the “Calcari a radiolitidi” (Radiolitid Limestone) Formation. This work is based on three stratigraphic sections from the Turonian interval of the ACP: Monte Coccovello (85 m), Raia del Pedale (110 m), and Monte Varchera (110 m). The late Cenomanian facies...
FIGURES
First thumbnail for: BENTHIC FORAMINIFERA IN THE AFTERMATH OF THE CENOM...
Second thumbnail for: BENTHIC FORAMINIFERA IN THE AFTERMATH OF THE CENOM...
Third thumbnail for: BENTHIC FORAMINIFERA IN THE AFTERMATH OF THE CENOM...
Journal Article
Journal: Geology
Published: 01 September 2008
Geology (2008) 36 (9): 715–718.
... of rotaliporids in the open ocean, and to link the biological crisis in carbonate platforms to changes in sea-surface temperature and ocean circulation and/or upwelling during OAE 2. Three sections in the southern Apennines (Italy) were selected for this study: Raia del Pedale, Monte Varchera, and Monte...
FIGURES
First thumbnail for: Stepwise extinction of larger foraminifers at the ...
Second thumbnail for: Stepwise extinction of larger foraminifers at the ...