Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3067
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dc.contributor.authorallFlorindo, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallKarner, D. B.; Department of Geology, Sonoma State University, 1801 East Cotati Avenue, Rohnert Park, CA 94985, USAen
dc.contributor.authorallMarra, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2007-12-11T12:08:04Zen
dc.date.available2007-12-11T12:08:04Zen
dc.date.issued2007en
dc.identifier.urihttp://hdl.handle.net/2122/3067en
dc.description.abstractBuried sedimentary aggradational sections deposited between 800 ka and 600 ka in the Tiber River coastal alluvial plain have been studied using borecores from around Rome. 40Ar/39Ar ages on sanidine and/or leucite from intercalated tephra layers and paleomagnetic investigation of clay sections provide geochronologic constraints on the timing of aggradation of two alluvial sections, demonstrating that they were deposited in response to glacio–eustatic sea level rise caused by Glacial Terminations IX and VII. 40Ar/39Ar age data indicate ages of 802±8 ka (1σ full errors) and 649±3 ka (1σ full errors) for Glacial Terminations IX and VII, respectively, providing a rare test, beyond the range of U-series dating for corals and speleothems (∼500 ka), of the astronomically calibrated timescale developed for oxygen isotope records from deep sea cores.en
dc.language.isoEnglishen
dc.publisher.nameelsevieren
dc.relation.ispartofEarth and Planetary Science Lettersen
dc.relation.ispartofseries/ 256 (2007)en
dc.subjectglacial terminationen
dc.subjectsea levelen
dc.subject40Ar/39Aren
dc.subjectTiber River deltaen
dc.subjectpaleomagnetismen
dc.titleRadioisotopic age constraints for Glacial Terminations IX and VII from aggradational sections of the Tiber River delta in Rome, Italyen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber61-80en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.02. Geochronologyen
dc.identifier.doi10.1016/j.epsl.2007.01.014en
dc.description.obiettivoSpecifico2.2. Laboratorio di paleomagnetismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorFlorindo, F.en
dc.contributor.authorKarner, D. B.en
dc.contributor.authorMarra, F.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentDepartment of Geology, Sonoma State University, 1801 East Cotati Avenue, Rohnert Park, CA 94985, USAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.cerifentitytypePublications-
item.grantfulltextrestricted-
item.openairetypearticle-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
item.languageiso639-1en-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione AC, Roma, Italia-
crisitem.author.deptDepartment of Geology, Sonoma State University-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-6058-9748-
crisitem.author.orcid0000-0002-4881-9563-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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