Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3849
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dc.contributor.authorallVilla, G.; Dipartimento di Scienze della Terra, Università di Parmaen
dc.contributor.authorallLupi, C.; Dipartimento di Scienze della Terra, Università di Paviaen
dc.contributor.authorallCobianchi, M.; Dipartimento di Scienze della Terra, Università di Paviaen
dc.contributor.authorallFlorindo, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallPekar, S. F.; Lamont-Doherty Earth Observatoryof ColumbiaUniversity, Palisades, NewYorken
dc.date.accessioned2008-05-13T08:30:03Zen
dc.date.available2008-05-13T08:30:03Zen
dc.date.issued2008en
dc.identifier.urihttp://hdl.handle.net/2122/3849en
dc.description.abstractBio- and magnetostratigraphic age data and nannofossil assemblage analysis from ODP Site 1165 evidence an anomalous warming event of the surface waters in and around Prydz Bay during the Early Pleistocene, approximately 1 Ma. This results from an increase in the abundance of nannofossils at Site 1165, that occurred at 1 Ma. Detailed high-resolution sampling permits a new bio-magnetostratigraphic interpretation for ODP Site 1165. A decrease in δ18O values at Sites 1165 and 1167 also occurs at this time, supporting the presence of warming conditions in the Prydz Bay area. A return to colder surface waters, indicated by the absence or rare occurrence of nannofossils in the upper cores from Site 1165, suggests that more stable glacial conditions existed in the Prydz Bay basin, for the last 900 ka. The biogenic carbonate sequence identified at Site 1167 is similar to the carbonate shales recovered from the Cape Roberts Project 1. Both have been dated at about 1 Ma, supporting the idea that a significant surface waters warming occurred during the Pleistocene. These data and the presence of calcareous nannofossils from locations around the Antarctic continent also suggest that the warming event was not limited to the analysed basin, but it extended around the East Antarctic continent. These new evidence call for a re-evaluation of the notion that the East Antarctic Ice-Sheet has experienced stable conditions similar to today since the late Neogene.en
dc.language.isoEnglishen
dc.publisher.nameELSEVIERen
dc.relation.ispartofPalaeogeography, Palaeoclimatology, Palaeoecologyen
dc.relation.ispartofseries1-2 / 260 (2008)en
dc.subjectANTARCTICAen
dc.titleA Pleistocene warming event at 1 Ma in Prydz Bay, East Antarctica: Evidence from ODP Site 1165en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber230-244en
dc.identifier.URLhttp://www.sciencedirect.com/science/journal/00310182en
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatologyen
dc.identifier.doi10.1016/j.palaeo.2007.08.017en
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dc.description.obiettivoSpecifico2.2. Laboratorio di paleomagnetismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorVilla, G.en
dc.contributor.authorLupi, C.en
dc.contributor.authorCobianchi, M.en
dc.contributor.authorFlorindo, F.en
dc.contributor.authorPekar, S. F.en
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Parmaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Paviaen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Paviaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentLamont-Doherty Earth Observatoryof ColumbiaUniversity, Palisades, NewYorken
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartimento di Scienze della Terra, Universita di Parma, Parco Aeres delle Scienze, 157 Parma, Italy-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Pavia-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Pavia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione AC, Roma, Italia-
crisitem.author.deptSchool of Earth and Environmental Sciences, Queens College, City University of New York, Flushing, New York 11367, USA-
crisitem.author.orcid0000-0002-6058-9748-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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