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)

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Fältnamn	Indikatorer	Metadata
000		04297naa a2200445 4500
001		oai:lup.lub.lu.se:1fb1dce0-d196-4312-8133-c53e9e3bb452
003		SwePub
008		221028s2022 \| \|\|\|\|\|\|\|\|\|\|\|000 \|\|eng\|
024	7	a https://lup.lub.lu.se/record/1fb1dce0-d196-4312-8133-c53e9e3bb4522 URI
024	7	a https://doi.org/10.1130/2022.2557(16)2 DOI
040		a (SwePub)lu
041		a engb eng
042		9 SwePub
072	7	a kap2 swepub-publicationtype
072	7	a ref2 swepub-contenttype
100	1	a Coccioni, Rodolfou University of Urbino4 aut
245	1 0	a 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)
264	1	b Geological Society of America,c 2022
520		a 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.
650	7	a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geologi0 (SwePub)105042 hsv//swe
650	7	a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geology0 (SwePub)105042 hsv//eng
700	1	a Montanari, Alessandrou Geological Observatory of Coldigioco (OGC)4 aut
700	1	a Boschi, Samueleu Lund University,Lunds universitet,Kärnfysik,Fysiska institutionen,Institutioner vid LTH,Lunds Tekniska Högskola,Nuclear physics,Department of Physics,Departments at LTH,Faculty of Engineering, LTH4 aut0 (Swepub:lu)nucl-smb
700	1	a Catanzariti, Ritau CNR: National Research Council of Italy4 aut
700	1	a Frontalini, Fabriziou University of Urbino4 aut
700	1	a Jovane, Luigiu University of São Paulo4 aut
700	1	a Kochhann, Marcus Vinicius Lermenu Federal University of Rio Grande do Sul4 aut
700	1	a Pelosi, Nicolau CNR: National Research Council of Italy4 aut
700	1	a Sabatino, Nadiau CNR: National Research Council of Italy4 aut
700	1	a Savian, Jairo F.u Federal University of Rio Grande do Sul4 aut
700	1	a Sprovieri, Mariou CNR: National Research Council of Italy4 aut
700	1	a Koeberl, Christian4 edt
700	1	a Claeys, Philippe4 edt
700	1	a Montanari, Alessandro4 edt
710	2	a University of Urbinob Geological Observatory of Coldigioco (OGC)4 org
773	0	t 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 Alvarezd : Geological Society of Americag 557q 557x 0072-1077z 9780813725574z 9780813795577
856	4	u http://dx.doi.org/10.1130/2022.2557(16)y FULLTEXT
856	4	u https://doi.org/10.1130/spe.s.18789311
856	4 8	u https://lup.lub.lu.se/record/1fb1dce0-d196-4312-8133-c53e9e3bb452
856	4 8	u https://doi.org/10.1130/2022.2557(16)

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