georefid:2007-087737georefid:2007-087735SEDIS 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.208.205.2006<gco:CharacterString>Data report; terrigenous grain-size distributions at Sites 1263 and 1267; testing the applicability of Leg 208 sediments for eolian analysis</gco:CharacterString>2007-01-01publicationgeorefid:2007-087737doi:10.2973/odp.proc.sr.208.205.2006Nicolo, Micah J.Rice University, Department of Earth Science, Houston, TX, United StatesauthorDickens, Gerald RoyUniversity of California, Santa Cruz, United StatesauthorTexas A&M University, Ocean Drilling Program, College Station, TX, United StatespublisherdocumentDigitalIn: Kroon, Dick, Zachos, James C., Blum, Peter, Bowles, Julie, Gaillot, Philippe, Hasegawa, Takashi, Hathorne, Edmund C., Hodell, David A., Kelly, Daniel C., Jung, Ja-Hun, Keller, Susan M., Lee, Youn Soo, Leuschner, Dirk C., Liu Zhifei, Lohmann, Kyger C., Lourens, Lucas, Monechi, Simonetta, Nicolo, Micah, Raffi, Isabella, Riesselman, Christina, Roehl, Ursula, Schellenberg, Stephen A., Schmidt, Daniela, Sluijs, Appy, Thomas, Deborah, Thomas, Ellen, Vallius, Henry, Proceedings of the Ocean Drilling Program; scientific results; early Cenozoic extreme climates; the Walvis Ridge Transect; covering Leg 208 of the cruises of the drilling vessel JOIDES Resolution; Rio de Janeiro, Brazil, to Rio de Janeiro, Brazil; Sites 1262-1267; 6 March-6 May 2003208To date, the only Southern Hemisphere eolian grain-size record constructed for the early Paleogene comes from Deep Sea Drilling Project Site 215. Ten early Paleogene sediment samples from Site 215 were collected and processed to show that the existing eolian grain-size record at this site can be reproduced. Five samples each from Ocean Drilling Program Sites 1263 and 1267 were similarly examined to test the possibility of generating new Southern Hemisphere eolian grain-size records for the early Paleogene. Our results indicate that an eolian grain-size signal can be constructed at Walvis Ridge, although the record will be complicated by hemipelagic terrigenous inputs. Further, we assert that a record generated at a site located on the deep flanks of Walvis Ridge is particularly susceptible to hemipelagic influence.completedStratigraphyAtlantic OceanboreholesCenozoiccoresDeep Sea Drilling ProjectDSDP Site 215grain sizeIndian OceanLeg 208Leg 22lithostratigraphylower Paleogenemarine sedimentsmethodsOcean Drilling ProgramODP Site 1263ODP Site 1267Paleogenesample preparationsedimentssize distributionSouth AtlanticSoutheast Atlanticterrigenous materialsTertiaryWalvis Ridgewind transporturn:org.iodp:exp:208urnlargerWorkCitationcampaignurn:org.iodp:exp:22urnlargerWorkCitationcampaignurn:org.iodp:exp:22:site:215urnlargerWorkCitationstudyurn:org.iodp:exp:22urnlargerWorkCitationcampaignurn:org.iodp:exp:208:site:1263urnlargerWorkCitationstudyurn:org.iodp:exp:208urnlargerWorkCitationcampaignurn:org.iodp:exp:208:site:1267urnlargerWorkCitationstudyurn:org.iodp:exp:208urnlargerWorkCitationcampaignEnglishgeoscientificInformation1.420086.4730-28.3200-8.0718Includes appendicesapplication/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://www-odp.tamu.edu/publications/208_SR/VOLUME/CHAPTERS/205.PDFdownload