georefid:2005-075249georefid:2005-075244SEDIS 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.ir.188.105.2001<gco:CharacterString>Site 1167</gco:CharacterString>2001-01-01publicationgeorefid:2005-075249doi:10.2973/odp.proc.ir.188.105.2001Cooper, Alan K.Stanford University, Department of Geological and Environmental Sciences, Stanford, CA, United StatesauthorO'Brien, Philip E.Australian Geological Survey Organisation, AustraliaauthorRichter, CarlOcean Drilling Program, United StatesauthorBarr, Samantha R.University of Leicester, United KingdomauthorBohaty, Steven M.University of Nebraska, United StatesauthorClaypool, George A.University of Texas at Arlington, United StatesauthorDamuth, John E.Oxford University, United KingdomauthorErwin, Patrick S.Istituto Nazionale di Geofisica, ItalyauthorFlorindo, FabioNorwegian Polar Institute, NorwayauthorForsberg, Carl FredrikChristan-Albrechts-Universitaet zu Kiel, Federal Republic of GermanyauthorGruetzner, JensUniversity of Utah, United StatesauthorHandwerger, David A.University of Toronto at Scarborough, CanadaauthorJanuszczak, Nicole N.Curtin University, AustraliaauthorKaiko, AlexanderBoston University, United StatesauthorKryc, Kelly A.British Antarctic Survey, United KingdomauthorLavelle, MarkOhio State University, United StatesauthorPasschier, SandraFlorida State University, United StatesauthorPospichal, James J.University of Tasmania, AustraliaauthorQuilty, Patrick G.Osservatorio Geofisico Sperimentale, ItalyauthorRebesco, Michele A.University of Oulu, FinlandauthorStrand, Kari O.Jacques Whitford and Associates, CanadaauthorTaylor, BrianCalifornia State University, United StatesauthorTheissen, Kevin M.Lamont-Doherty Earth Observatory, United StatesauthorWarnke, Detlef A.Australian Geological Survey, AustraliaauthorWhalen, Patricia A.Ocean Drilling Program, United StatesauthorWhitehead, Jason M.University of Leicester, United KingdomauthorWilliams, TrevorUniversity of Nebraska, United StatesauthorTexas A&M University, Ocean Drilling Program, College Station, TX, United StatespublisherdocumentDigitalIn: Cooper, Alan K., O'Brien, Philip E., Richter, Carl, Barr, Samantha R., Bohaty, Steven M., Claypool, George E., Damuth, John E., Erwin, Patrick S., Florindo, Fabio, Forsberg, Carl Fredrik, Gruetzner, Jens, Handwerger, David A., Januszczak, Nicole N., Kaiko, Alexander, Kryc, Kelly A., Lavelle, Mark, Passchier, Sandra, Pospichal, James J., Quilty, Patrick G., Rebesco, Michele A., Strand, Kari O., Taylor, Brian, Theissen, Kevin M., Warnke, Detlef A., Whalen, Patricia A., Whitehead, Jason M., Williams, Trevor, Peters, Lorri L. (editor), Proceedings of the Ocean Drilling Program; initial reports; Prydz Bay-Cooperation Sea, Antarctica; glacial history and paleoceanography; covering Leg 188 of the cruises of the drilling vessel JOIDES Resolution; Fremantle, Australia, to Hobart, Tasmania; Sites 1165-1167; 10 January-11 March 2000188The Amery Ice Shelf-Lambert Glacier ice drainage system drains about 22% of the East Antarctic Ice Sheet (EAIS); therfore, Lambert Glacier responds to fluctuations in the EAIS. It is the objective of this chapter to investigate which glacial episodes throughout late Neogene time produced a major advance and what paleoenvironmental conditions existed when the major advance occurred. The best location to find answers to these questions is in the trough mouth fan, which received siliciclastic sediment from the ice front when the shelf eroded during major ice advances and depositied hemispelagic material during interglacials and smaller glaciations. Site 1167 was located in the middle of the Prydz Channel Fan with the intent of drilling through a section that was reasonably complete without being so close to the shelf edge that it would have been affected by large-scale sluping. Models of trough mouth fan sedimentation suggest that thick siliciclastic units should correspond to peaks in Antarctic ice volume, wheras periods of reduced ice volume should be represented by hemipelagic sediments.completedQuaternary geologyalgaeAntarcticabiostratigraphyCenozoicclimate changeCooperation Seacoresdepositional environmentdiatomsdownhole methodsForaminiferageochemistryHoloceneInvertebrataLeg 188lithostratigraphymicrofossilsnannofossilsOcean Drilling ProgramODP Site 1167paleoclimatologypaleomagnetismphysical propertiesPlantaePleistoceneProtistaPrydz BayQuaternaryRadiolariasedimentationsedimentation ratesSouthern Oceanurn:org.iodp:exp:188urnlargerWorkCitationcampaignurn:org.iodp:exp:188:site:1167urnlargerWorkCitationstudyurn:org.iodp:exp:188urnlargerWorkCitationcampaignEnglishgeoscientificInformation72.170072.1700-66.2400-66.2400Includes appendix; available only on CD-ROM in PDF format and on the Web in PDF or HTMLapplication/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://www-odp.tamu.edu/publications/188_IR/VOLUME/CHAPTERS/IR188_05.PDFdownload