georefid:2003-022409georefid:2003-022395SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.2973/odp.proc.sr.178.233.2001<gco:CharacterString>The magnetic mineral assemblage of hemipelagic drifts, ODP Site 1096</gco:CharacterString>2002-01-01publicationgeorefid:2003-022409doi:10.2973/odp.proc.sr.178.233.2001Brachfeld, Stefanie A.University of Minnesota, Department of Geology and Geophysics, Minneapolis, MN, United StatesauthorGuyodo, Yohan J. B.Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, ItalyauthorActon, Gary D.Ocean Drilling Program, United StatesauthorTexas A&M University, Ocean Drilling Program, College Station, TX, United StatespublisherdocumentDigitalIn: Baker, Peter F. (editor), Camerlenghi, Angelo (editor), Acton, Gary D. (editor), Brachfeld, Stefanie A., Cowan, Ellen A., Daniels, James, Domack, Eugene W., Escutia, Carlota, Evans, Andrew J., Eyles, Nicholas, Guyodo, Yohan J. B., Hatfield, Kate L., Iorio, Marina, Iwai, Masao, Kyte, Frank T., Lauer, Christine, Maldonado, Andres, Moerz, Tobias, Osterman, Lisa E., Pudsey, Carol J., Schuffert, Jeffrey D., Sjunneskog, Charlotte M., Weinheimer, Amy L., Williams, Trevor, Winter, Diane M., Wolf-Welling, Thomas C. W., Ramsay, Anthony T. S. (editor), Proceedings of the Ocean Drilling Program, scientific results, Antarctic glacial history and sea-level change; covering Leg 178 of the cruises of the drilling vessel JOIDES Resolution; Punta Arenas, Chile, to Cape Town, South Africa; sites 1095-1103; 5 February-9 April 1998178During Ocean Drilling Program (ODP) Leg 178, we drilled three sites on sediment drifts deposited on the continental rise on the western margin of the Antarctic Peninsula. These hemipelagic drifts were targeted for their potential to preserve a continuous record of the behavior of the West Antarctic Ice Sheet over the last 10 m.y. It has been proposed that drift development is linked to advances and retreats of the Antarctic continental ice sheet (Pudsey and Camerlenghi, 1998, and references therein; Barker, Camerlenghi, Acton, et al., 1999). However, the sediment is characterized by a very low carbonate content, with foraminifers restricted to very narrow intervals. This lack of carbonate precludes the construction of a O-18/O-16 or CaCO (sub 3) stratigraphy, depriving these sites of an important chronologic tool and global ice volume proxy.completedStratigraphyAntarctic OceanAntarctic PeninsulaAntarcticabiostratigraphyCenozoicclastic sedimentscoresdriftForaminiferahemipelagic environmentInvertebrataisotope ratiosisotopesLeg 178magnetic mineralsmagnetostratigraphymarine environmentmarine sedimentsmicrofossilsmineral assemblagesNeogeneO-18/O-16Ocean Drilling Programocean floorsODP Site 1096oxygenpaleomagnetismPlioceneProtistaQuaternarysedimentsstable isotopesTertiaryurn:org.iodp:exp:178urnlargerWorkCitationcampaignurn:org.iodp:exp:178:site:1096urnlargerWorkCitationstudyurn:org.iodp:exp:178urnlargerWorkCitationcampaignEnglishgeoscientificInformation-76.5749-76.5749-67.3401-67.3401Data report; available only on CD-ROM in PDF format and on the Web in PDF or HTML; access date Feb. 24, 2002application/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://www-odp.tamu.edu/publications/178_SR/VOLUME/CHAPTERS/SR178_14.PDFdownload