Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7031
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dc.contributor.authorallCapraro, L.; Department of Geosciences, Via Gradenigo 6, I-35100 Padova, Italyen
dc.contributor.authorallMassari, F.; Department of Geosciences, Via Gradenigo 6, I-35100 Padova, Italyen
dc.contributor.authorallRio, D.; Department of Geosciences, Via Gradenigo 6, I-35100 Padova, Italyen
dc.contributor.authorallFornaciari, E.; Department of Geosciences, Via Gradenigo 6, I-35100 Padova, Italyen
dc.contributor.authorallBackman, J.; Department of Geology and Geochemistry, S-10691 Stockholm, Swedenen
dc.contributor.authorallChannell, J. E. T.; Department of Geological Sciences, POB 112120, Gainesville, FL-32611, USAen
dc.contributor.authorallMacrì, P.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallProsser, G.; Department of Geological Sciences, Campus Macchiaromana I-85100 Potenza, Italyen
dc.contributor.authorallSperanza, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.date.accessioned2011-06-14T06:40:41Zen
dc.date.available2011-06-14T06:40:41Zen
dc.date.issued2011-05en
dc.identifier.urihttp://hdl.handle.net/2122/7031en
dc.description.abstractBiostratigraphy based on calcareous nannofossils, integrated by magnetostratigraphic, geochronological and isotopic data, allowed establishing a precise chronological framework for the Pleistocene succession within the south-western sector of the Crotone Basin (Calabria, Southern Italy), where the Pliocenee Pleistocene global stratotype section and point is defined, thus demonstrating that sedimentation was quasi-continuous during most of the Lower and Middle Pleistocene. At a large scale, the Pleistocene succession in this sector of the Crotone Basin is characterized by an evident shallowing-upwards trend, showing facies changes from bathyal to shelfal to littoral/continental. However, comparison between adjacent sectors within the investigated area demonstrates that stratigraphic architectures change vastly on very short distances. Our chronological constraints indicate that such changes in sedimentation styles probably occurred in response to differential subsidence rates, which originated tectonically-controlled synsedimentary structures where accommodation space and sediment yield were allotted unevenly. This articulated physiography led to striking differences in the overall thicknesses and organization of Pleistocene stratigraphies and, eventually, to a distinct diachroneity in the first appearance of shallow-marine deposits. In addition, superimposed are complex interplays between regional and local tectonics, eustasy and orbitally-forced climate changes. These interactions have been highlighted by the oxygen isotope stratigraphy established for a part of the studied succession, which is likely to document almost continuously the interval from Marine Isotope Stage (MIS) 26 to MIS 17. In its younger part (post-MIS 17), chronological ties are poor, as the succession is dominated by shallow-water to continental deposits showing a prominent organization into cyclothems. Nevertheless, based on the chronology of the underlying units, it is feasible that basin infill ended during MIS 15-MIS 14 times.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofQuaternary Science Reviewsen
dc.relation.ispartofseries9-10/30(2011)en
dc.subjectPleistoceneen
dc.subjectChronostratigraphyen
dc.subjectSouthern Italyen
dc.titleChronology of the Lower-Middle Pleistocene succession of the south-western part of the Crotone Basin (Calabria, Southern Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1185-1200en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transporten
dc.subject.INGV04. Solid Earth::04.05. Geomagnetism::04.05.06. Paleomagnetismen
dc.identifier.doi10.1016/j.quascirev.2011.02.008en
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dc.description.obiettivoSpecifico2.2. Laboratorio di paleomagnetismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.contributor.authorCapraro, L.en
dc.contributor.authorMassari, F.en
dc.contributor.authorRio, D.en
dc.contributor.authorFornaciari, E.en
dc.contributor.authorBackman, J.en
dc.contributor.authorChannell, J. E. T.en
dc.contributor.authorMacrì, P.en
dc.contributor.authorProsser, G.en
dc.contributor.authorSperanza, F.en
dc.contributor.departmentDepartment of Geosciences, Via Gradenigo 6, I-35100 Padova, Italyen
dc.contributor.departmentDepartment of Geosciences, Via Gradenigo 6, I-35100 Padova, Italyen
dc.contributor.departmentDepartment of Geosciences, Via Gradenigo 6, I-35100 Padova, Italyen
dc.contributor.departmentDepartment of Geosciences, Via Gradenigo 6, I-35100 Padova, Italyen
dc.contributor.departmentDepartment of Geology and Geochemistry, S-10691 Stockholm, Swedenen
dc.contributor.departmentDepartment of Geological Sciences, POB 112120, Gainesville, FL-32611, USAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentDepartment of Geological Sciences, Campus Macchiaromana I-85100 Potenza, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartment of Geosciences, Via Gradenigo 6, I-35100 Padova, Italy-
crisitem.author.deptDepartment of Geosciences, Via Gradenigo 6, I-35100 Padova, Italy-
crisitem.author.deptDepartment of Geology and Geochemistry, S-10691 Stockholm, Sweden-
crisitem.author.deptDepartment of Geological Sciences, POB 112120, Gainesville, FL-32611, USA-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptDepartment of Geological Sciences, Campus Macchiaromana I-85100 Potenza, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.orcid0000-0003-1718-2106-
crisitem.author.orcid0000-0001-7369-9535-
crisitem.author.orcid0000-0003-2287-4019-
crisitem.author.orcid0000-0001-5492-8670-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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