Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4827
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dc.contributor.authorallGiaccio, B.; Istituto di Geologia ambientale e Geoingegneria, CNR, Via Bolognola 7, 00138 Rome, Italyen
dc.contributor.authorallIsaia, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallFedele, F. G.; Laboratorio di Antropologia, Dipartimento delle Scienze biologiche, Università di Napoli “Federico II”, Naples, Italyen
dc.contributor.authorallDi Canzio, E.; Dipartimento di Scienze della Terra, Università di Roma “La Sapienza”, Rome, Italyen
dc.contributor.authorallHoffecker, J.; Institute of Arctic and Alpine Research, University of Colorado, Boulder, USAen
dc.contributor.authorallRonchitelli, A.; Dipartimento di Archeologia e Storia delle Arti, Università di Pisa, Pisa, Italyen
dc.contributor.authorallSinitsyn, A. A.; Institute of the History of Material Culture, Russian Academy of Sciences, Petersburg, Russiaen
dc.contributor.authorallAnikovich, M.; Institute of the History of Material Culture, Russian Academy of Sciences, Petersburg, Russiaen
dc.contributor.authorallLisitsyn, S.; Institute of the History of Material Culture, Russian Academy of Sciences, Petersburg, Russiaen
dc.contributor.authorallPopov, V. V.en
dc.date.accessioned2008-12-15T22:21:57Zen
dc.date.available2008-12-15T22:21:57Zen
dc.date.issued2008en
dc.identifier.urihttp://hdl.handle.net/2122/4827en
dc.description.abstractTephra layers from archaeological sites in southern Italy and eastern Europe stratigraphically associated with cultural levels containing Early Upper Palaeolithic industry were analysed. The results confirm the occurrence of the Campanian Ignimbrite tephra (CI; ca. 40 cal ka BP) at Castelcivita Cave (southern Italy), Temnata Cave (Bulgaria) and in the Kostenki–Borshchevo area of the Russian Plain. This tephra, originated from the largest eruption of the Phlegrean Field caldera, represents the widest volcanic deposit and one of the most important temporal/stratigraphic markers of western Eurasia. At Paglicci Cave and lesser sites in the Apulia region we recognise a chemically and texturally different tephra, which lithologically, chronologically and chemically matches the physical and chemical characteristics of the Plinian eruption of Codola; a poorly known Late Pleistocene explosive event from the Neapolitan volcanoes, likely Somma–Vesuvius. For this latter, we propose a preliminary age estimate of ca. 33 cal ka BP and a correlation to the widespread C-10 marine tephra of the central Mediterranean. The stratigraphic position of both CI and Codola tephra layers at Castelcivita and Paglicci help date the first and the last documented appearance of Early Upper Palaeolithic industries of southern Italy to ca. 41–40 and 33 cal ka BP, respectively, or between two interstadial oscillations of the Monticchio pollen record – to which the CI and Codola tephras are physically correlated – corresponding to the Greenland interstadials 10–9 and 5. In eastern Europe, the stratigraphic and chronometric data seem to indicate an earlier appearance of the Early Upper Palaeolithic industries, which would predate of two millennia at least the overlying CI tephra. The tephrostratigraphic correlation indicates that in both regions the innovations connected with the so-called Early Upper Palaeolithic – encompassing subsistence strategy and stone tool technology – appeared and evolved during one of the most unstable climatic phases of the Last Glacial period. On this basis, the marked environmental unpredictability characterising this time-span is seen as a potential ecological factor involved in the cultural changes observed.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofJournal of Volcanology and Geothermal Researchen
dc.relation.ispartofseries/177(2008)en
dc.subjectCampanian Ignimbriteen
dc.subjectEarly Upper Palaeolithicen
dc.subjectCodola Plinian eruptionen
dc.subjectsouth-eastern Europeen
dc.titleThe Campanian Ignimbrite and Codola tephra layers: Two temporal/stratigraphic markers for the Early Upper Palaeolithic in southern Italy and eastern Europeen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber208–226en
dc.identifier.URLhttp://hdl.handle.net/2122/2883en
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocksen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risken
dc.subject.INGV05. General::05.02. Data dissemination::05.02.03. Volcanic eruptionsen
dc.identifier.doi10.1016/j.jvolgeores.2007.10.007en
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dc.description.obiettivoSpecifico3.5. Geologia e storia dei sistemi vulcanicien
dc.description.obiettivoSpecifico3.6. Fisica del vulcanismoen
dc.description.obiettivoSpecifico4.3. TTC - Scenari di pericolosità vulcanicaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorGiaccio, B.en
dc.contributor.authorIsaia, R.en
dc.contributor.authorFedele, F. G.en
dc.contributor.authorDi Canzio, E.en
dc.contributor.authorHoffecker, J.en
dc.contributor.authorRonchitelli, A.en
dc.contributor.authorSinitsyn, A. A.en
dc.contributor.authorAnikovich, M.en
dc.contributor.authorLisitsyn, S.en
dc.contributor.authorPopov, V. V.en
dc.contributor.departmentIstituto di Geologia ambientale e Geoingegneria, CNR, Via Bolognola 7, 00138 Rome, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentLaboratorio di Antropologia, Dipartimento delle Scienze biologiche, Università di Napoli “Federico II”, Naples, Italyen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Roma “La Sapienza”, Rome, Italyen
dc.contributor.departmentInstitute of Arctic and Alpine Research, University of Colorado, Boulder, USAen
dc.contributor.departmentDipartimento di Archeologia e Storia delle Arti, Università di Pisa, Pisa, Italyen
dc.contributor.departmentInstitute of the History of Material Culture, Russian Academy of Sciences, Petersburg, Russiaen
dc.contributor.departmentInstitute of the History of Material Culture, Russian Academy of Sciences, Petersburg, Russiaen
dc.contributor.departmentInstitute of the History of Material Culture, Russian Academy of Sciences, Petersburg, Russiaen
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crisitem.author.deptCNR - IGAG-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptUniversità di Roma "La Sapienza", Dipartimento di Scienze della Terra-
crisitem.author.deptInstitute of Arctic and Alpine Research, University of Colorado, Boulder, USA-
crisitem.author.deptDipartimento di Archeologia e Storia delle Arti, Università di Pisa, Pisa, Italy-
crisitem.author.deptInstitute of the History of Material Culture, Russian Academy of Sciences, Petersburg, Russia-
crisitem.author.deptInstitute of the History of Material Culture, Russian Academy of Sciences, Petersburg, Russia-
crisitem.author.deptInstitute of the History of Material Culture, Russian Academy of Sciences, Petersburg, Russia-
crisitem.author.orcid0000-0001-7277-2358-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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