Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/3559
DC Field | Value | Language |
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dc.contributor.authorall | Lirer, F.; Istituto per l'Ambiente Marino Costiero (IAMC) - CNR sede di Napoli, Italy | en |
dc.contributor.authorall | Cascella, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.authorall | Cesarano, M.; Dipartimento S.T.A.T., Università del Molise, Pesche (Isernia), Italy | en |
dc.contributor.authorall | Casciello, E.; Dipartimento S.T.A.T., Università del Molise, Pesche (Isernia), Italy | en |
dc.contributor.authorall | Pappone, G.; Dipartimento S.T.A.T., Università del Molise, Pesche (Isernia), Italy | en |
dc.date.accessioned | 2008-02-15T08:40:05Z | en |
dc.date.available | 2008-02-15T08:40:05Z | en |
dc.date.issued | 2007-07 | en |
dc.identifier.uri | http://hdl.handle.net/2122/3559 | en |
dc.description.abstract | A biostratigraphic study was carried out on four sections of the Miocene Tufillo and Faeto formations (Southern Apennines). The sediments analysed were referred to the late Burdigalian - early Tortonian on the basis of planktonic foraminifers (MMi2b Sub-zone through the MMi8 Zone) and calcareous nannofossils (MNN3b Zone through the MNN7 Zone). Almost the majority of the bioevents of the recently published Miocene biozonal schemes of Mediterranean area were identified. Particularly, the marked changes in the abundance pattern of Paragloborotalia siakensis resulted very useful to correlate the sediments. A new acme abundance of the letter species has been recorded in the uppermost part of the Burdigalian planktonic foraminiferal EMMi2b Subzone. Moreover, the integrated calcareous plankton biostratigraphy revealed that the First Common Occurrence (FCO) of Sphenolithus heteromorphus occurs before the Last Occurrence (LO) of Catapsidrax dissimilis, in the upper part of Burdigalian record. This study indicates that the lower Langhian portion of the Tufillo Formation is characterized by arkose sandstones which pass upwards into calcarenites and/or calcirudites and marly deposits. Field data suggest that these sandstones directly overly the "Numidian Sandstones". The Faeto Formation starts with calcarenites and calcareous marls, in the calcareous nannofossil MNN3b Zone (Burdigalian), and lies on the "Numidian Standstones" as well. High-resolution sampling and biostratigraphy reveal that the deposition of the "Numidian Sandstones" ends in the late Burdigalian stage, just below the FCO of S.heteromorphus (MNN3b Zone) and the LO of C.dissimilis (MMi2b Subzone). | en |
dc.language.iso | English | en |
dc.publisher.name | Dipartimento di Scienze della Terra, Università degli Studi di Milano | en |
dc.relation.ispartof | Rivista Italiana di Paleontologia e Stratigrafia | en |
dc.relation.ispartofseries | 2 / 113 (2007) | en |
dc.subject | Calcareous plankton biostratigraphy | en |
dc.subject | Early and Middle Miocene | en |
dc.subject | Mediterranean | en |
dc.subject | Faeto Formation | en |
dc.subject | Tufillo Formation | en |
dc.subject | Southern Apennines | en |
dc.title | Micropaleontological study on the Miocene calcareous turbidite deposits of Faeto and Tufillo formations (eastern sector of the Southern Apennine chain) | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 269-286 | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transport | en |
dc.subject.INGV | 04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy | en |
dc.description.obiettivoSpecifico | 2.2. Laboratorio di paleomagnetismo | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | reserved | en |
dc.contributor.author | Lirer, F. | en |
dc.contributor.author | Cascella, A. | en |
dc.contributor.author | Cesarano, M. | en |
dc.contributor.author | Casciello, E. | en |
dc.contributor.author | Pappone, G. | en |
dc.contributor.department | Istituto per l'Ambiente Marino Costiero (IAMC) - CNR sede di Napoli, Italy | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.department | Dipartimento S.T.A.T., Università del Molise, Pesche (Isernia), Italy | en |
dc.contributor.department | Dipartimento S.T.A.T., Università del Molise, Pesche (Isernia), Italy | en |
dc.contributor.department | Dipartimento S.T.A.T., Università del Molise, Pesche (Isernia), Italy | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto per l’Ambiente Marino Costiero, Consiglio Nazionale delle Ricerche, Calata Porta di Massa, Interno Porto di Napoli, 80133 Naples, Italy | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia | - |
crisitem.author.dept | Institut de Ciencies de la Terra “Jaume Almera”, CSIC, Barcelona, Spain | - |
crisitem.author.orcid | 0000-0003-4938-3252 | - |
crisitem.author.orcid | 0000-0002-8255-3244 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
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Lirer et al. 2007.pdf | 8.04 MB | Adobe PDF |
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