Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4017
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dc.contributor.authorallFlorindo, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallCooper, A. K.; Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USAen
dc.contributor.authorallO'Brien, P. E.; Geoscience Australia, G.P.O. Box 378, Canberra, ACT 2601, Australiaen
dc.date.accessioned2008-08-28T12:52:54Zen
dc.date.available2008-08-28T12:52:54Zen
dc.date.issued2003-09-15en
dc.identifier.urihttp://hdl.handle.net/2122/4017en
dc.description.abstractThe Antarctic region has profoundly affected the global climates of the past 50 million years, influencing sea levels, atmospheric composition and dynamics, and ocean circulation. A greater understanding of this region and the Antarctic cryosphere is crucial to a broader understanding of the global climates and palaeoceanography at all scales. Much of the information obtained during the last two decades derives from studies of sedimentary sequences drilled in and around Antarctica. Eight Ocean Drilling Program (ODP) legs have contributed significantly to the understanding of this evolution. These legs include Leg 113 in the Weddell Sea (Barker et al., 1988, 1990), Leg 114 in the Subantarctic South Atlantic (Ciesielski et al., 1988, 1991), Leg 119 in Prydz Bay and on Kerguelen Plateau (Barron et al., 1989, 1991), Leg 120 on Kerguelen Plateau (Schlich et al., 1989; Wise et al., 1992), Leg 177 in the southeast Atlantic sector of the Southern Ocean (Gersonde et al., 1999), Leg 178 on the Antarctic Peninsula (Barker et al., 2002), Leg 188 in Prydz Bay (O’Brien et al., 2001), and Leg 189 in the Tasmanian region (Exon et al., 2001). More recently, a series of three holes were drilled in McMurdo Sound, Ross Sea, as part of the Cape Roberts Project (CRP; Cape Roberts Science Team, 1998 1999, 2000; Hambrey et al., 1998; Barrett et al., 2000, 2001). In spite of these efforts, which have significantly advanced our understanding of the Cenozoic tectonics and palaeoenvironments of the Antarctic region, important questions and problems remain unresolved. Chief amongst these are the timing of the onset of the East Antarctic Ice Sheet (EAIS), the causes of the cooling events at around 24 and 14 Ma, and the warming events of the mid-Pliocene and Marine Isotope Stages 31 (1.07 Ma) and 11 (0.36 Ma) (Shackleton et al., 1995).en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofPalaeogeography, Palaeoclimatology, Palaeoecologyen
dc.relation.ispartofseries1 / 198 (2003)en
dc.subjectAntarctic climate evolutionen
dc.titleIntroduction to ‘Antarctic Cenozoic palaeoenvironments: geologic record and models’en
dc.typearticleen
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.identifier.doi10.1016/S0031-0182(03)00405-Xen
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dc.description.obiettivoSpecifico3.8. Geofisica per l'ambienteen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorFlorindo, F.en
dc.contributor.authorCooper, A. K.en
dc.contributor.authorO'Brien, P. E.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentDepartment of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USAen
dc.contributor.departmentGeoscience Australia, G.P.O. Box 378, Canberra, ACT 2601, Australiaen
item.fulltextWith Fulltext-
item.languageiso639-1en-
item.cerifentitytypePublications-
item.openairetypearticle-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextrestricted-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione AC, Roma, Italia-
crisitem.author.deptDepartment of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA-
crisitem.author.deptustralian Geological Survey Organization, Canberra, Australia-
crisitem.author.orcid0000-0002-6058-9748-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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