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Monte Coccovello

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<b>Monte</b> <b>Coccovello</b> section: lithological–sedimentological log, oxygen- and ca...

Monte Coccovello section: lithological–sedimentological log, oxygen- and ca...

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 ...

Schematic geological map of the southern Apennines (modified from Bonardi ...

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 δ 13 C ...

Comparison with the Eastbourne Chalk curve shows that pre-excursion δ 13 C ...

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 stand...

Chemostratigraphic correlation of the three studied sections with the stand...

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

Carbon-isotope stratigraphy of Cenomanian–Turonian platform carbonates from the southern Apennines (Italy): a chemostratigraphic approach to the problem of correlation between shallow-water and deep-water successions

Published: 01 May 2007
Journal of the Geological Society (2007) 164 (3): 609–620.
DOI: https://doi.org/10.1144/0016-76492006-010
...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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Journal Article

BENTHIC FORAMINIFERA IN THE AFTERMATH OF THE CENOMANIAN-TURONIAN BOUNDARY EXTINCTION EVENT IN THE CARBONATE PLATFORM FACIES OF THE SOUTHERN APENNINES (ITALY)

Published: 01 January 2016
Journal of Foraminiferal Research (2016) 46 (1): 9–24.
DOI: https://doi.org/10.2113/gsjfr.46.1.9
... interval of the ACP: Monte Coccovello (85 m), Raia del Pedale (110 m), and Monte Varchera (110 m). The late Cenomanian facies evolution, biostratigraphy and carbon-isotope stratigraphy of these sections has been described in previous papers ( Parente et al., 2007 ; Frijia & Parente, 2008a , b...
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Journal Article

Stepwise extinction of larger foraminifers at the Cenomanian-Turonian boundary: A shallow-water perspective on nutrient fluctuations during Oceanic Anoxic Event 2 (Bonarelli Event)

Journal: Geology
Published: 01 September 2008
Geology (2008) 36 (9): 715–718.
DOI: https://doi.org/10.1130/G24893A.1
... Apennines (Italy) were selected for this study: Raia del Pedale, Monte Varchera, and Monte Coccovello. The stratigraphic ranges of larger foraminifers were determined by careful logging in the field and by the study of more than 300 thin sections. Samples for carbon isotope stratigraphy were taken...
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