georefid:2010-053861SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-07-06T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=2010-053861<gco:CharacterString>A view of Antarctic ice-sheet evolution from sea-level and deep-sea isotope changes during the Late Cretaceous-Cenozoic</gco:CharacterString>2007-01-01publicationgeorefid:2010-053861Miller, K. G.Rutgers University, Department of Earth and Planetary Sciences, Piscataway, NJ, United StatesauthorWright, J. D.Jet Propulsion Laboratory, United StatesauthorKatz, M. E.University of Oregon, United StatesauthorBrowning, J. V.Texas A&M University, United StatesauthorCramer, B. S.authorWade, B. S.authorMizintseva, S. F.authorU. S. Geological Survey, Reston, VA, United StatespublisherdocumentDigitalIn: Cooper, Alan (editor), Raymond, Carol (editor), Antarctica; a keystone in a changing world; online proceedings for the 10th international symposium on Antarctic earth sciencesOF 2007-104755-70The imperfect direct record of Antarctic glaciation has led to the delayed recognition of the initiation of a continent-sized ice sheet. Early studies interpreted initiation in the middle Miocene (ca 15 Ma). Most current studies place the first ice sheet in the earliest Oligocene (33.55 Ma), but there is physical evidence for glaciation in the Eocene. Though there are inherent limitations in sea-level and deep-sea isotope records, both place constraints on the size and extent of Late Cretaceous to Cenozoic Antarctic ice sheets. Sea-level records argue that small- to medium-size (typically 10-12X10 (super 6) km (super 3) ) ephemeral ice sheets occurred during the greenhouse world of the Late Cretaceous to middle Eocene. Deep-sea delta (super 18) O records show increases associated with many of these greenhouse sea-level falls, consistent with their attribution to ice-sheet growth. Global cooling began in the middle Eocene and culminated with the major earliest Oligocene (33.55 Ma) growth of a large (25X10 (super 6) km (super 3) ) Antarctic ice sheet that caused a 55-70 m eustatic fall and a 1% delta (super 18) O increase. This large ice sheet became a driver of climate change, not just a response to it, causing increased latitudinal thermal gradients and a spinning up of the oceans that, in turn, caused a dramatic reorganization of ocean circulation and chemistry.completedStratigraphyAntarctic ice sheetAntarcticaCenozoicclimate changecorrelationCretaceousdeep-sea environmentEast PacificEoceneEquatorial PacificForaminiferaglacial geologyice sheetsIndian OceanInvertebrataisotope ratiosisotopesKerguelen PlateauLeg 119Leg 120Leg 199marine environmentMesozoicmicrofossilsMioceneNeogeneNorth PacificNortheast PacificO-18/O-16Ocean Drilling ProgramODP Site 1218OligoceneoxygenPacific Oceanpaleo-oceanographypaleoclimatologyPaleogeneProtistareconstructionsea-level changesSouthern Oceanstable isotopesTertiaryUSGSurn:org.iodp:exp:119urnlargerWorkCitationcampaignurn:org.iodp:exp:120urnlargerWorkCitationcampaignurn:org.iodp:exp:199urnlargerWorkCitationcampaignurn:org.iodp:exp:199:site:1218urnlargerWorkCitationstudyurn:org.iodp:exp:199urnlargerWorkCitationcampaignEnglishgeoscientificInformation-180.0000180.0000-90.000025.0000AntarcticaIndian OceanKerguelen PlateauSouthern OceanAccessed on May 27, 2010application/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://pubs.usgs.gov/of/2007/1047/10th_ISAES_Table_1.pdfdownload