georefid:2005-041676georefid:2005-041660SEDIS 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.182.008.2002<gco:CharacterString>Trace element geochemistry of Cenozoic cool-water carbonates, Sites 1126-1132, Great Australian Bight</gco:CharacterString>2004-01-01publicationgeorefid:2005-041676doi:10.2973/odp.proc.sr.182.008.2002Emmanuel, LaurentUniversite de Bourgogne, Centre des Sciences de la Terre, Dijon, FranceauthorRobin, CecileAustralian Geological Survey Organisation, AustraliaauthorRenard, MauriceTexas A&M University, United StatesauthorTexas A&M University, Ocean Drilling Program, College Station, TX, United StatespublisherdocumentDigitalIn: Hine, Albert C., Feary, David A., Malone, Mitchell J., Andres, Miriam, Betzler, Christian, Brooks, Gregg R., Brunner, Charlotte A., Fuller, Michael, Molina Garza, Roberto S., Holbourn, Ann E., Huuse, Mads, Isern, Alexandra R., James, Noel P., Ladner, Bryan C., Li, Qianyu, Machiyama, Hideaki, Mallinson, David J., Matsuda, Hiroki, Mitterer, Richard M., Robin, Cecile, Russell, Joellen L., Shafik, Samir, Simo, J. A., Smart, Peter L., Spence, Guy H., Surlyk, Finn C., Swart, Peter K., Wortmann, Ulrich G., Proceedings of the Ocean Drilling Program; scientific results; Great Australian Bight; Cenozoic cool-water carbonates; covering Leg 182 of the cruises of the drilling vessel JOIDES Resolution; Wellington, New Zealand, to Fremantle, Australia; Sites 1126-1134, 8 October-7 December 1998182An intensive geochemical investigation was conducted on carbonate sediments recovered during Ocean Drilling Program Leg 182. Four trace elements in 635 sediment samples from Sites 1126-1132 on the Great Australian Bight were examined by atomic absorption spectrometry on the acid-soluble fraction. Downhole profiles of these elements exhibit complicated fluctuations throughout the late Eocene to Pleistocene, principally because of the variations in the acid-soluble fraction. The purpose of this study is to present initial results on the geochemical composition of Cenozoic cool-water carbonates as a basis for a future detailed investigation to determine the paleoenvironment of a carbonate-dominated continental margin during the evolution of the Southern Ocean.completedGeochemistry of rocks, soils, and sedimentsOceanographyalgaeatomic absorption spectraAustralasiaAustraliabiostratigraphybiozonescarbonate sedimentscarbonatesCenozoiccoresForaminiferageochemistryGreat Australian BightIndian OceanInvertebrataLeg 182lithostratigraphymarine sedimentsmicrofossilsnannofossilsOcean Drilling Programocean floorspaleoenvironmentPlantaeProtistasedimentsspectratrace elementsurn:org.iodp:exp:182urnlargerWorkCitationcampaignEnglishgeoscientificInformation127.1500128.5500-34.2330-33.1720Available only on CD-ROM in PDF format and on the Web in PDF or HTML; data reportapplication/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://www-odp.tamu.edu/publications/182_SR/VOLUME/CHAPTERS/008.PDFdownload