Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5197
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dc.contributor.authorallMuttoni, G.; Università di Milanoen
dc.contributor.authorallScardia, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Milano-Pavia, Milano, Italiaen
dc.contributor.authorallKent, D. V.; Lamont-Doherty Earth Observatoryen
dc.contributor.authorallSwisher, C. C.; Rutgers Universityen
dc.contributor.authorallManzi, G.; Università di Roma "La Sapienza"en
dc.date.accessioned2009-10-14T14:03:13Zen
dc.date.available2009-10-14T14:03:13Zen
dc.date.issued2009en
dc.identifier.urihttp://hdl.handle.net/2122/5197en
dc.description.abstractPaleomagnetic analyses were conducted on two cores drilled at Ceprano in central Italy where an incomplete hominin cranium was discovered in1994, as well as on two additional cores from the nearby site of Fontana Ranuccio that yielded hominin remains associated with an Acheulean industry. No evidence for the 0.78 Ma Brunhes–Matuyama boundary was found at Ceprano down to 45 m below the level that yielded the hominin cranium. The Ceprano lithostratigraphy and the paleomagnetic age constraints are broadly consistent with the stratigraphy of the Liri lacustrine sequence of the Latina Valley, constrained by published K–Ar ages between ~0.6 and ~0.35Ma, and according to an age model with magnetic susceptibility supported by pollen facies data, suggest that the level that yielded the hominin cranium has an age of ~0.45 (+0.05, −0.10) Ma. Evidence for the Brunhes–Matuyama boundary was found at Fontana Ranuccio about 40 m below the hominin level, consistent with a K–Ar age of ~0.46 Ma reported for this level. Hence the Ceprano and Fontana Ranuccio hominin occurrences may be of very similar mid-Brunhes age.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofEarth and Planetray Science Lettersen
dc.relation.ispartofseries/286 (2009)en
dc.subjectPleistoceneen
dc.subjectCepranoen
dc.subjectFontana Ranuccioen
dc.subjectmagnetostratigraphyen
dc.subjecthomininsen
dc.subjectItalyen
dc.titlePleistocene magnetochronology of early hominin sites at Ceprano and Fontana Ranuccio, Italyen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber255-268en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.10. Stratigraphyen
dc.identifier.doi10.1016/j.epsl.2009.06.032en
dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorMuttoni, G.en
dc.contributor.authorScardia, G.en
dc.contributor.authorKent, D. V.en
dc.contributor.authorSwisher, C. C.en
dc.contributor.authorManzi, G.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Milano, Milano, Italiaen
dc.contributor.departmentLamont-Doherty Earth Observatoryen
dc.contributor.departmentRutgers Universityen
dc.contributor.departmentUniversità di Roma "La Sapienza"en
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptInstituto Oceanográfico, Universidade de São Paulo, São Paulo, Brazil-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Milano, Milano, Italia-
crisitem.author.deptUniversità di Roma "La Sapienza"-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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