Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4025
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dc.contributor.authorallVenuti, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallCobianchi, M.; Dipartimento di Scienze della Terra, Università degli Studi di Pavia, Pavia, Italyen
dc.contributor.authorallLupi, C.; Dipartimento di Scienze della Terra, Università degli Studi di Pavia, Pavia, Italyen
dc.contributor.editorallTewles, K. B.; Nova Science Publishers, Inc.en
dc.date.accessioned2008-09-02T06:40:35Zen
dc.date.available2008-09-02T06:40:35Zen
dc.date.issued2008en
dc.identifier.isbn978-1-60692-010-7en
dc.identifier.urihttp://hdl.handle.net/2122/4025en
dc.description.abstractPaleoclimatic proxies from sedimentary marine sequences often record orbital frequencies (eccentricity, obliquity, and precession) and reveal the effects of insolation on environmental processes. During Pleistocene an important transition occurred in the time interval between 1.25 and 0.7 Ma, the so called Mid-Pleistocene Transition (MPT; Clark et al., 2006) that marked the passage from glacial cycles with 41 to 100-kyr rhythm. In the southwestern Pacific Ocean this transition reflects in paleoceanographic changes as the case east of New Zealand in correspondence of the northward flow of the Deep Western Boundary Current (DWBC). Many studies show evidences of the MPT by the use of proxies dependent on bulk and magnetic sediment grain-size and which provide qualitative information on variations in the strength of the deep Pacific Ocean inflow, possibly directly related to fluctuations of Antarctic Bottom Water production. Many works have been performed about these topics which revealed the importance to improve and enhance the knowledge through future researches.en
dc.language.isoEnglishen
dc.publisher.nameNova Science Publishers, Inc.en
dc.relation.ispartofThe Pacific and Arctic Oceans: new Oceanographis Researchen
dc.subjectPleistoceneen
dc.subjectPacific Oceanen
dc.subjectclimate changeen
dc.titleRecords of Climate and Paleoceanographic Variability during the Mid-Pleistocene Transition in the Pacific Oceanen
dc.title.alternativeShort Communicationsen
dc.typebook chapteren
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1-9en
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatologyen
dc.description.obiettivoSpecifico2.2. Laboratorio di paleomagnetismoen
dc.description.obiettivoSpecifico3.8. Geofisica per l'ambienteen
dc.description.fulltextreserveden
dc.contributor.authorVenuti, A.en
dc.contributor.authorCobianchi, M.en
dc.contributor.authorLupi, C.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università degli Studi di Pavia, Pavia, Italyen
dc.contributor.departmentDipartimento di Scienze della Terra, Università degli Studi di Pavia, Pavia, Italyen
dc.contributor.editorTewles, K. B.en
dc.contributor.editordepartmentNova Science Publishers, Inc.en
item.openairetypebook chapter-
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 Roma2, Roma, Italia-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Pavia-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Pavia-
crisitem.author.orcid0000-0002-0213-3355-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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