georefid:2006-075594georefid:2006-075590SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.2973/odp.proc.sr.194.004.20042006-01-01publicationgeorefid:2006-075594doi:10.2973/odp.proc.sr.194.004.2004Page, Michael C.James Cook University, School of Ocean Sciences, Townsville, Queensl., AustraliaauthorTexas A&M University, Ocean Drilling Program, College Station, TX, United StatespublisherdocumentDigitalIn: Anselmetti, Flavio S., Isern, Alexandra R., Blum, Peter, Andresen, Nils, Birke, Tesfaye Kidane, Bracco Gartner, Guido L., Burns, Stephen J., Conesa, Gilles A. R., Delius, Heike, Dugan, Brandon, Eberli, Gregor P., Ehrenberg, Stephen N., Fuller, Michael D., Muller, Pamela Hallock, Hine, Albert C., Howell, Michael W., John, Cedric M., Karner, Garry D., Kindler, Pascal F., Olson, Brooke E., Sasaki, Keiichi, Stewart, Duncan, Wei, Wuchang, White, Timothy S., Wood, Jason L., Yamada, Tsutomu, Proceedings of the Ocean Drilling Program; constraining Miocene sea level change from carbonate platform evolution, Marion Plateau, northeast Australia; covering Leg 194 of the cruises of the drilling vessel JOIDES Resolution; Townsville, Australia, to Apra Harbor, Guam; Sites 1192-1199; 3 January-2 March 2001194Upper Quaternary sediment sequences east of the Great Barrier Reef are characterized by alternating siliciclastic- and carbonate-rich horizons caused by changes in the input of various sedimentary components and reflected in cores by variations in bulk carbonate content. A total of 153 measurements of bulk carbonate content were determined using the carbonate-bomb technique for late Pleistocene sediments between 0 and 23.69 meters below sea floor (mbsf) in Ocean Drilling Program Hole 1198A. Average sample resolution was 15 cm and multiple analyses were performed on each sample. Bulk carbonate content ranges from a maximum of 94 wt% at 13.63 mbsf to a minimum of 73 wt% at 14.54 mbsf. Five cyclic trends are observed that may relate to five major glacial events during the last 500 k.y. of the Quaternary.completedQuaternary geologycarbonatesCenozoicCoral Seacoresdepositional environmentGreat Barrier ReefLeg 194marine sedimentsOcean Drilling ProgramODP Site 1198Pacific Oceanpaleo-oceanographypaleoclimatologypaleoenvironmentQuaternarysedimentssiliciclasticsSouth PacificSouthwest Pacificupper QuaternaryvariationsWest Pacificurn:org.iodp:exp:194urnlargerWorkCitationcampaignurn:org.iodp:exp:194:site:1198urnlargerWorkCitationstudyurn:org.iodp:exp:194urnlargerWorkCitationcampaignEnglishgeoscientificInformation152.4300152.4500-20.5800-20.5700Data report; available only on CD-ROM in PDF format and on the Web in PDF or HTMLapplication/pdfunknownSEDIS Publication Catalogue

ana.macario@awi.de

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