georefid:2009-038469SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.2204/iodp.proc.311.211.2009<gco:CharacterString>Data report; Diatom and foraminiferal assemblages in Pleistocene turbidite sediments from the Cascadia margin (IODP Expedition 311), Northeast Pacific</gco:CharacterString>2009-01-01publicationgeorefid:2009-038469doi:10.2204/iodp.proc.311.211.2009Akiba, FumioDiatom Minilab Akiba, Hanno, JapanauthorInoue, YokoU. S. Geological Survey, United StatesauthorSaito-Kato, MegumiIntegrated Ocean Drilling Program, United StatesauthorPohlman, JohnLamont-Doherty Earth Observatory, United StatesauthorIODP Management International, Washington, DC, United StatespublisherdocumentDigitalIn: Riedel, Michael, Collett, Timothy S., Malone, Mitchell J., Guerin, Gilles, Akiba, Fumio, Blanc-Valleron, Marie-Madeleine, Ellis, Michelle, Hashimoto, Yoshitaka, Heuer, Verena, Higashi, Yosuke, Holland, Melanie, Jackson, Peter D., Kaneko, Masanori, Kastner, Miriam, Kim, Ji-Hoon, Kitajima, Hiroko, Long, Philip E., Malinverno, Alberto, Myers, Greg, Palekar, Leena D., Pohlman, John, Schultheiss, Peter, Teichert, Barbara, Torres, Marta E., Trehu, Anne M., Wang Jiasheng, Wortmann, Ulrich G., Yoshioka, Hideyoshi, Proceedings of the Integrated Ocean Drilling Program; Cascadia margin gas hydrates; Expedition 311 of the riserless drilling platform; Balboa, Panama, to Victoria, British Columbia (Canada); Sites U1325-U1329, 28 August-28 October 2005311Diatom and foraminiferal analyses of the Pleistocene turbidites in the Cascadia margin suggest that turbidite sediments originated mainly in the landward shelf area and were displaced to the present deep-sea site, which maintained a constant depth during this time. Abundant and highly fluctuating occurrences of shallowmarine and nonmarine diatoms may reflect the global glacioeustatic sea level changes in the Pleistocene.completedQuaternary geologyalgaeassemblagesbiostratigraphyboreholesCascadia subduction zoneCenozoicclastic sedimentscoresdepositional environmentdiatomsEast PacificExpedition 311Foraminiferafresh-water environmentIntegrated Ocean Drilling ProgramInvertebrataIODP Site 1325IODP Site 1326IODP Site 1327IODP Site 1328IODP Site 1329marine environmentmarine sedimentsmicrofossilsNorth PacificNortheast PacificPacific OceanPlantaePleistoceneProtistaQuaternarysedimentationsedimentation ratessedimentsSEM datasporesturbiditeurn:org.iodp:exp:311urnlargerWorkCitationcampaignurn:org.iodp:exp:311:site:U1325urnlargerWorkCitationstudyurn:org.iodp:exp:311urnlargerWorkCitationcampaignurn:org.iodp:exp:311:site:U1326urnlargerWorkCitationstudyurn:org.iodp:exp:311urnlargerWorkCitationcampaignurn:org.iodp:exp:311:site:U1327urnlargerWorkCitationstudyurn:org.iodp:exp:311urnlargerWorkCitationcampaignurn:org.iodp:exp:311:site:U1328urnlargerWorkCitationstudyurn:org.iodp:exp:311urnlargerWorkCitationcampaignurn:org.iodp:exp:311:site:U1329urnlargerWorkCitationstudyurn:org.iodp:exp:311urnlargerWorkCitationcampaignEnglishgeoscientificInformation-127.0400-126.400048.370048.4800application/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://publications.iodp.org/proceedings/311/ERR/CHAPTERS/311_211.PDFdownload