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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).

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

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
Image
 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.

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

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.
Image
 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).

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

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.

Chemostratigraphic correlation of the three studied sections with the stand... Available to Purchase

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 Available to Purchase

Mariano Parente, Gianluca Frijia, Matteo Di Lucia
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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View PDF for article title, 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
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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) Available to Purchase

Maria Eugenia Arriaga, Gianluca Frija, Mariano Parente, Esmeralda Caus
Published: 01 January 2016
Journal of Foraminiferal Research (2016) 46 (1): 9–24.
DOI: https://doi.org/10.2113/gsjfr.46.1.9
... 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...
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View PDF for article title, BENTHIC FORAMINIFERA IN THE AFTERMATH OF THE CENOMANIAN-TURONIAN BOUNDARY EXTINCTION EVENT IN THE CARBONATE PLATFORM FACIES OF THE SOUTHERN APENNINES (ITALY)
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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) Available to Purchase

Mariano Parente, Gianluca Frijia, Matteo Di Lucia, Hugh C. Jenkyns, Richard G. Woodfine, Francesco Baroncini
Journal: Geology
Published: 01 September 2008
Geology (2008) 36 (9): 715–718.
DOI: https://doi.org/10.1130/G24893A.1
... 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...
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View PDF for article title, Stepwise extinction of larger foraminifers at the Cenomanian-Turonian boundary: A shallow-water perspective on nutrient fluctuations during Oceanic Anoxic Event 2 (Bonarelli Event)
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Add to Citation Manager for Stepwise extinction of larger foraminifers at the Cenomanian-Turonian boundary: A shallow-water perspective on nutrient fluctuations during Oceanic Anoxic Event 2 (Bonarelli Event)