georefid:2003-022415georefid: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.178.220.2001<gco:CharacterString>Oxygen and carbon isotope measurements on Neogloboquadrina pachyderma (s) from holes 1096B and 1101A, Antarctic Peninsula margin, Leg 178</gco:CharacterString>2002-01-01publicationgeorefid:2003-022415doi:10.2973/odp.proc.sr.178.220.2001Barker, Peter F.British Antarctic Survey, Cambridge, United KingdomauthorOsterman, Lisa E.Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, ItalyauthorHall, Michael A.Ocean Drilling Program, United StatesauthorTexas A&M University, Ocean Drilling Program, College Station, TX, United StatespublisherdocumentDigitalIn: Barker, 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 1998178Oxygen and carbon isotopic ratios were measured on left-coiling Neogloboquadrina pachyderma separated from sediments recovered from Holes 1096B (3152 m water depth) and 1101A (3280 m water depth) during Ocean Drilling Program Leg 178. The sediment samples were widely spaced, extending over the past 2.1 m.y. The nature of the sediments from which they were separated and the measured oxygen isotopic ratios show that N. pachyderma (s) is preserved in both glacial and interglacial sediments over the entire period, pointing to the possibility of extracting a detailed isotopic record at these sites extending back to 2.1 Ma.completedQuaternary geologyAntarctic OceanAntarctic PeninsulaAntarcticaC-13/C-12carbonCenozoiccontinental margincoresdepositional environmentForaminiferaGlobigerinaceaInvertebrataisotope ratiosisotopesLeg 178marine sedimentsmicrofossilsNeogloboquadrinaNeogloboquadrina pachydermaO-18/O-16Ocean Drilling Programocean floorsODP Site 1096ODP Site 1101oxygenpaleoclimatologypaleoenvironmentPleistoceneProtistaQuaternaryreconstructionRotaliinasedimentsstable isotopesurn:org.iodp:exp:178urnlargerWorkCitationcampaignurn:org.iodp:exp:178:site:1096urnlargerWorkCitationstudyurn:org.iodp:exp:178urnlargerWorkCitationcampaignurn:org.iodp:exp:178:site:1101urnlargerWorkCitationstudyurn:org.iodp:exp:178urnlargerWorkCitationcampaignEnglishgeoscientificInformation-76.5749-70.1540-67.3401-64.2220Data 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_20.PDFdownload