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Integrated stratigraphy of the Lutetian-Priabonian pelagic section at Bottaccione (Gubbio, central Italy) : A proposal for defining and positioning the Global Stratotype Section and Point (GSSP) for the base of the Bartonian Stage (Paleogene System, Eocene Series)

Coccioni, Rodolfo ; Montanari, Alessandro ; Boschi, Samuele LU ; Catanzariti, Rita ; Frontalini, Fabrizio ; Jovane, Luigi ; Kochhann, Marcus Vinicius Lermen ; Pelosi, Nicola ; Sabatino, Nadia and Savian, Jairo F. , et al. (2022) In Special Paper of the Geological Society of America 557.
Abstract

At present, the Global Stratotype Section and Point (GSSP) for the base of the Bartonian remains the only GSSP of the Paleogene System to be defined by the International Subcommission on Paleogene Stratigraphy (ISPS) and the International Commission on Stratigraphy (ICS). Here, we present the results of an integrated, high-resolution study of calcareous plankton and benthic foraminifera biostratigraphy and a detailed magneto-, chemo-, and cyclostratigraphic analyses carried out through the upper Lutetian to the upper Priabonian pelagic sediments of the Bottaccione Gorge section near Gubbio, central Italy, to check its stratigraphic completeness and constrain in time the optimal interval for defining and positioning the GSSP for the base... (More)

At present, the Global Stratotype Section and Point (GSSP) for the base of the Bartonian remains the only GSSP of the Paleogene System to be defined by the International Subcommission on Paleogene Stratigraphy (ISPS) and the International Commission on Stratigraphy (ICS). Here, we present the results of an integrated, high-resolution study of calcareous plankton and benthic foraminifera biostratigraphy and a detailed magneto-, chemo-, and cyclostratigraphic analyses carried out through the upper Lutetian to the upper Priabonian pelagic sediments of the Bottaccione Gorge section near Gubbio, central Italy, to check its stratigraphic completeness and constrain in time the optimal interval for defining and positioning the GSSP for the base of the Bartonian Stage. The high-resolution and solid integrated stratigraphic framework established at Bottaccione confirmed the completeness of the section, which meets the ICS recommendations for a potential designation as a GSSP for the base of the Bartonian Stage. Thus, the Bottaccione section was compared with the parastratotype section of the Bartonian in its type area, Alum Bay, UK. On this basis, two reliable criteria for defining and positioning the Bartonian GSSP at Bottaccione are provided: (1) the base of magnetic polarity chronozone C18r as the primary correlation criterion and (2) the base of the calcareous nannofossil Dictyococcites bisectus, which defines the CNE14/CNE15 zonal boundary as a secondary correlation criterion.

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publishing date
type
Chapter in Book/Report/Conference proceeding
publication status
published
subject
host publication
From the Guajira Desert to the Apennines, and from Mediterranean Microplates to the Mexican Killer Asteroid : Honoring the Career of Walter Alvarez - Honoring the Career of Walter Alvarez
series title
Special Paper of the Geological Society of America
editor
Koeberl, Christian ; Claeys, Philippe and Montanari, Alessandro
volume
557
publisher
Geological Society of America
external identifiers
  • scopus:85135460682
ISSN
0072-1077
ISBN
9780813725574
9780813795577
DOI
10.1130/2022.2557(16)
language
English
LU publication?
yes
id
1fb1dce0-d196-4312-8133-c53e9e3bb452
date added to LUP
2022-10-28 14:38:14
date last changed
2024-04-04 13:05:41
@inbook{1fb1dce0-d196-4312-8133-c53e9e3bb452,
  abstract     = {{<p>At present, the Global Stratotype Section and Point (GSSP) for the base of the Bartonian remains the only GSSP of the Paleogene System to be defined by the International Subcommission on Paleogene Stratigraphy (ISPS) and the International Commission on Stratigraphy (ICS). Here, we present the results of an integrated, high-resolution study of calcareous plankton and benthic foraminifera biostratigraphy and a detailed magneto-, chemo-, and cyclostratigraphic analyses carried out through the upper Lutetian to the upper Priabonian pelagic sediments of the Bottaccione Gorge section near Gubbio, central Italy, to check its stratigraphic completeness and constrain in time the optimal interval for defining and positioning the GSSP for the base of the Bartonian Stage. The high-resolution and solid integrated stratigraphic framework established at Bottaccione confirmed the completeness of the section, which meets the ICS recommendations for a potential designation as a GSSP for the base of the Bartonian Stage. Thus, the Bottaccione section was compared with the parastratotype section of the Bartonian in its type area, Alum Bay, UK. On this basis, two reliable criteria for defining and positioning the Bartonian GSSP at Bottaccione are provided: (1) the base of magnetic polarity chronozone C18r as the primary correlation criterion and (2) the base of the calcareous nannofossil Dictyococcites bisectus, which defines the CNE14/CNE15 zonal boundary as a secondary correlation criterion.</p>}},
  author       = {{Coccioni, Rodolfo and Montanari, Alessandro and Boschi, Samuele and Catanzariti, Rita and Frontalini, Fabrizio and Jovane, Luigi and Kochhann, Marcus Vinicius Lermen and Pelosi, Nicola and Sabatino, Nadia and Savian, Jairo F. and Sprovieri, Mario}},
  booktitle    = {{From the Guajira Desert to the Apennines, and from Mediterranean Microplates to the Mexican Killer Asteroid : Honoring the Career of Walter Alvarez}},
  editor       = {{Koeberl, Christian and Claeys, Philippe and Montanari, Alessandro}},
  isbn         = {{9780813725574}},
  issn         = {{0072-1077}},
  language     = {{eng}},
  month        = {{06}},
  publisher    = {{Geological Society of America}},
  series       = {{Special Paper of the Geological Society of America}},
  title        = {{Integrated stratigraphy of the Lutetian-Priabonian pelagic section at Bottaccione (Gubbio, central Italy) : A proposal for defining and positioning the Global Stratotype Section and Point (GSSP) for the base of the Bartonian Stage (Paleogene System, Eocene Series)}},
  url          = {{http://dx.doi.org/10.1130/2022.2557(16)}},
  doi          = {{10.1130/2022.2557(16)}},
  volume       = {{557}},
  year         = {{2022}},
}