Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8301
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dc.contributor.authorallZanchetta, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallGiraudi, C.; ENEA, C.R. Saluggia, 13040 Vercelli, Italyen
dc.contributor.authorallSulpizio, R.; CIRISIVU, c/o Dipartimento Geomineralogico, University of Bari, 70125, Bari, Italyen
dc.contributor.authorallDrysdale, R. N.; Department of Resource Management and Geography, University of Melbourne, Victoria 3010, Australiaen
dc.contributor.authorallSadori, L.; Dipartimento di Biologia Vegetale, Università “La Sapienza”, 00185 Roma, Italyen
dc.date.accessioned2012-10-19T13:09:48Zen
dc.date.available2012-10-19T13:09:48Zen
dc.date.issued2012-09en
dc.identifier.urihttp://hdl.handle.net/2122/8301en
dc.description.abstractA study of six tephra layers discovered in different deposits between 1600 and 2700 m a.s.l. in the Apennine chain in central Italy allowed precise stratigraphic constraints on environmental and climatic changes between ca. 4.5 and 3.8 cal ka BP. Chemical analyses allowed the correlation of these tephra layers with the eruptions of Agnano Mt Spina (AMST) from Phlegrean Field and Avellino (AVT) from Somma–Vesuvius. Major environmental changes in the high mountains of the Central Apennines occurred just after the deposition of the AMST and predate the deposition of the AVT. At this time, renewed growth of the Calderone Glacier occurred, marking the onset of the Apennine “Neoglacial”. The presence of the AMST and AVT enabled us to make a precise, physical correlation with other archives in central Italy. Synchronization of records between sites showed that the period intervening the deposition of the AMST and AVT layers coincided with environmental changes that were not always exactly in phase. This highlights the fact that stratigraphic correlations using only radiocarbon chronologies (the most common method used for dating archives during the Holocene) could produce erroneous correlation of events, giving rise to oversimplified paleoclimatic reconstructions.en
dc.language.isoEnglishen
dc.publisher.nameElsevier Science Limiteden
dc.relation.ispartofQuaternary Researchen
dc.relation.ispartofseries2/78(2012)en
dc.subjectTephrostratigraphyen
dc.subjectHoloceneen
dc.subjectCentral Italyen
dc.subjectPaleoclimateen
dc.titleConstraining the onset of the Holocene “Neoglacial” over the central Italy using tephra layersen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber236-247en
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.99. General or miscellaneousen
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatologyen
dc.identifier.doi10.1016/j.yqres.2012.05.010en
dc.description.obiettivoSpecifico3.7. Dinamica del clima e dell'oceanoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn0033-5894en
dc.relation.eissn1096-0287en
dc.contributor.authorZanchetta, G.en
dc.contributor.authorGiraudi, C.en
dc.contributor.authorSulpizio, R.en
dc.contributor.authorDrysdale, R. N.en
dc.contributor.authorSadori, L.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentENEA, C.R. Saluggia, 13040 Vercelli, Italyen
dc.contributor.departmentCIRISIVU, c/o Dipartimento Geomineralogico, University of Bari, 70125, Bari, Italyen
dc.contributor.departmentDepartment of Resource Management and Geography, University of Melbourne, Victoria 3010, Australiaen
dc.contributor.departmentDipartimento di Biologia Vegetale, Università “La Sapienza”, 00185 Roma, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptENEA, C.R. Saluggia, 13040 Vercelli, Italy-
crisitem.author.deptCIRISIVU, c/o Dipartimento Geomineralogico, Universita' di Bari-
crisitem.author.orcid0000-0002-7080-9599-
crisitem.author.orcid0000-0002-3930-5421-
crisitem.author.orcid0000-0001-7867-031X-
crisitem.author.orcid0000-0002-2774-6705-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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