The global stratotype section and point (GSSP) for the base of the chattian stage (paleogene system, oligocene series) at monte cagnero, Italy

Rodolfo Coccioni; Alessandro Montanari; David Bice; Henk Brinkhuis; Alain Deino; Fabrizio Frontalini; Fabrizio Lirer; Patrizia Maiorano; Simonetta Monechi; Jörg Pross; Pierre Rochette; Leonardo Sagnotti; Marianna Sideri; Mario Sprovieri; Fabio Tateo; Yannick Touchard; Stefaan Van Simaeys; Graham L. Williams

doi:10.18814/epiiugs/2018/v41i1/018003

The global stratotype section and point (GSSP) for the base of the chattian stage (paleogene system, oligocene series) at monte cagnero, Italy

Rodolfo Coccioni, Alessandro Montanari, David Bice, Henk Brinkhuis, Alain Deino, Fabrizio Frontalini, Fabrizio Lirer, Patrizia Maiorano, Simonetta Monechi, Jörg Pross, Pierre Rochette, Leonardo Sagnotti, Marianna Sideri, Mario Sprovieri, Fabio Tateo, Yannick Touchard, Stefaan Van Simaeys, Graham L. Williams

Geosciences

Research output: Contribution to journal › Article › peer-review

18 Scopus citations

Abstract

The GSSP for the base of the Chattian Stage (Paleogene System, Oligocene Series) is defined at meter level 197 in the Monte Cagnero section, which belongs to the pelagic succession of the Umbria-Marche basin (Urbania, central Italy: 43°38′47.81″N-12°28′03.83″E). This level with an astronomical age of 27.82 Ma coincides with the highest common occurrence of the planktonic foraminifer Chiloguembelina cubensis at the base of planktonic foraminiferal O5 Zone and falls in the upper part of calcareous nannofossil NP24 Zone, in the lower part of dinocyst Dbi Zone, and in the lower Chron C9n. The proposal was approved by the International Subcommission of Paleogene Stratigraphy in July 2015, approved by the International Commission of Stratigraphy in August 2016, and ratified by the International Union of Geological Sciences in September 2016.

Original language	English (US)
Pages (from-to)	17-32
Number of pages	16
Journal	Episodes
Volume	41
Issue number	1
DOIs	https://doi.org/10.18814/epiiugs/2018/v41i1/018003
State	Published - Mar 2018

All Science Journal Classification (ASJC) codes

General Earth and Planetary Sciences

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10.18814/epiiugs/2018/v41i1/018003

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Coccioni, R., Montanari, A., Bice, D., Brinkhuis, H., Deino, A., Frontalini, F., Lirer, F., Maiorano, P., Monechi, S., Pross, J., Rochette, P., Sagnotti, L., Sideri, M., Sprovieri, M., Tateo, F., Touchard, Y., Van Simaeys, S., & Williams, G. L. (2018). The global stratotype section and point (GSSP) for the base of the chattian stage (paleogene system, oligocene series) at monte cagnero, Italy. Episodes, 41(1), 17-32. https://doi.org/10.18814/epiiugs/2018/v41i1/018003

@article{a13ad286a64f4abc9b445e58323ecfd9,

title = "The global stratotype section and point (GSSP) for the base of the chattian stage (paleogene system, oligocene series) at monte cagnero, Italy",

abstract = "The GSSP for the base of the Chattian Stage (Paleogene System, Oligocene Series) is defined at meter level 197 in the Monte Cagnero section, which belongs to the pelagic succession of the Umbria-Marche basin (Urbania, central Italy: 43°38′47.81″N-12°28′03.83″E). This level with an astronomical age of 27.82 Ma coincides with the highest common occurrence of the planktonic foraminifer Chiloguembelina cubensis at the base of planktonic foraminiferal O5 Zone and falls in the upper part of calcareous nannofossil NP24 Zone, in the lower part of dinocyst Dbi Zone, and in the lower Chron C9n. The proposal was approved by the International Subcommission of Paleogene Stratigraphy in July 2015, approved by the International Commission of Stratigraphy in August 2016, and ratified by the International Union of Geological Sciences in September 2016.",

author = "Rodolfo Coccioni and Alessandro Montanari and David Bice and Henk Brinkhuis and Alain Deino and Fabrizio Frontalini and Fabrizio Lirer and Patrizia Maiorano and Simonetta Monechi and J{\"o}rg Pross and Pierre Rochette and Leonardo Sagnotti and Marianna Sideri and Mario Sprovieri and Fabio Tateo and Yannick Touchard and {Van Simaeys}, Stefaan and Williams, {Graham L.}",

year = "2018",

month = mar,

doi = "10.18814/epiiugs/2018/v41i1/018003",

language = "English (US)",

volume = "41",

pages = "17--32",

journal = "Episodes",

issn = "0705-3797",

publisher = "International Union of Geological Sciences",

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Coccioni, R, Montanari, A, Bice, D, Brinkhuis, H, Deino, A, Frontalini, F, Lirer, F, Maiorano, P, Monechi, S, Pross, J, Rochette, P, Sagnotti, L, Sideri, M, Sprovieri, M, Tateo, F, Touchard, Y, Van Simaeys, S & Williams, GL 2018, 'The global stratotype section and point (GSSP) for the base of the chattian stage (paleogene system, oligocene series) at monte cagnero, Italy', Episodes, vol. 41, no. 1, pp. 17-32. https://doi.org/10.18814/epiiugs/2018/v41i1/018003

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T1 - The global stratotype section and point (GSSP) for the base of the chattian stage (paleogene system, oligocene series) at monte cagnero, Italy

AU - Coccioni, Rodolfo

AU - Montanari, Alessandro

AU - Bice, David

AU - Brinkhuis, Henk

AU - Deino, Alain

AU - Frontalini, Fabrizio

AU - Lirer, Fabrizio

AU - Maiorano, Patrizia

AU - Monechi, Simonetta

AU - Pross, Jörg

AU - Rochette, Pierre

AU - Sagnotti, Leonardo

AU - Sideri, Marianna

AU - Sprovieri, Mario

AU - Tateo, Fabio

AU - Touchard, Yannick

AU - Van Simaeys, Stefaan

AU - Williams, Graham L.

PY - 2018/3

Y1 - 2018/3

N2 - The GSSP for the base of the Chattian Stage (Paleogene System, Oligocene Series) is defined at meter level 197 in the Monte Cagnero section, which belongs to the pelagic succession of the Umbria-Marche basin (Urbania, central Italy: 43°38′47.81″N-12°28′03.83″E). This level with an astronomical age of 27.82 Ma coincides with the highest common occurrence of the planktonic foraminifer Chiloguembelina cubensis at the base of planktonic foraminiferal O5 Zone and falls in the upper part of calcareous nannofossil NP24 Zone, in the lower part of dinocyst Dbi Zone, and in the lower Chron C9n. The proposal was approved by the International Subcommission of Paleogene Stratigraphy in July 2015, approved by the International Commission of Stratigraphy in August 2016, and ratified by the International Union of Geological Sciences in September 2016.

AB - The GSSP for the base of the Chattian Stage (Paleogene System, Oligocene Series) is defined at meter level 197 in the Monte Cagnero section, which belongs to the pelagic succession of the Umbria-Marche basin (Urbania, central Italy: 43°38′47.81″N-12°28′03.83″E). This level with an astronomical age of 27.82 Ma coincides with the highest common occurrence of the planktonic foraminifer Chiloguembelina cubensis at the base of planktonic foraminiferal O5 Zone and falls in the upper part of calcareous nannofossil NP24 Zone, in the lower part of dinocyst Dbi Zone, and in the lower Chron C9n. The proposal was approved by the International Subcommission of Paleogene Stratigraphy in July 2015, approved by the International Commission of Stratigraphy in August 2016, and ratified by the International Union of Geological Sciences in September 2016.

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The global stratotype section and point (GSSP) for the base of the chattian stage (paleogene system, oligocene series) at monte cagnero, Italy

Abstract

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