georefid:2001-025827georefid:2001-025795SEDIS 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.164.244.2000<gco:CharacterString>Data report; (super 14) C dating of sediment of the uppermost Cape Fear Slide plain; constraints on the timing of this massive submarine landslide</gco:CharacterString>2000-01-01publicationgeorefid:2001-025827doi:10.2973/odp.proc.sr.164.244.2000Rodriguez, Nancy M.University of North Carolina at Chapel Hill, Department of Geology, Chapel Hill, NC, United StatesauthorPaull, Charles K.University of Tokyo, JapanauthorTexas A & M University, Ocean Drilling Program, College Station, TX, United StatespublisherdocumentHardcopyIn: Paull, Charles K., Matsumoto, Ryo, Wallace, Paul J., Black, Nancy R., Borowski, Walter S., Collett, Timothy S., Damuth, John E., Dickens, Gerald R., Egeberg, Per Kristian, Goodman, Kim, Hesse, Reinhard F., Hiroki, Yoshihisa, Holbrook, W. Steven, Hoskins, Hartley, Ladd, John, Lodolo, Emanuele, Lorenson, Thomas D., Musgrave, Robert J., Naehr, Thomas H., Okada, Hisatake, Pierre, Catherine, Ruppel, Carolyn D., Satoh, Mikio, Thiery, Regis, Watanabe, Yoshio, Wehner, Hermann, Winters, William J., Wood, Warren T., Miller, Christine M. (editor), Reigel, Ruth (editor), Proceedings of the Ocean Drilling Program; volume 164; scientific results; gas hydrate sampling on the Blake Ridge and Carolina Rise; covering Leg 164 of the cruises of the drilling vessel JOIDES Resolution, Halifax, Nova Scotia, to Miami, Florida, sites 991-997, 31 October-19 December 1995164325-327Six (super 14) C-age measurements of the carbonate fraction of sediments sampled from Ocean Drilling Program (ODP) Leg 164 Site 991 are reported. These samples straddle the most recent sole of the Cape Fear Slide. These data indicate that a hiatus occurs at 2.06 mbsf that separates sediments with (super 14) C ages < or =10 ka from those with ages > or =26.9 ka. The hiatus corresponds with a stratigraphic boundary between soft, undisturbed sediment above and firmer, yet disturbed sediment below, and is believed to correspond with the most recent activity on the slide.completedQuaternary geologyabsolute ageC-14Cape Fear ArchCape Fear SlidecarbonCenozoiccontinental margindatesHoloceneisotopesLeg 164marine sedimentsmass movementsNorth CarolinaOcean Drilling ProgramODP Site 991PleistoceneQuaternaryradioactive isotopessedimentsslumpingunconformitiesUnited Statesupper Pleistoceneurn:org.iodp:exp:164urnlargerWorkCitationcampaignurn:org.iodp:exp:164:site:991urnlargerWorkCitationstudyurn:org.iodp:exp:164urnlargerWorkCitationcampaignEnglishgeoscientificInformation-75.5548-75.554832.590132.5901