georefid:2004-034778SEDIS 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=2004-0347782003-01-01publicationgeorefid:2004-034778Fuller, M.University of Hawaii, HIGP-SOEST, Honolulu, HI, United StatesauthorMolina-Garza, R.Universidad Nacional Autonoma de Mexico, MexicoauthorAntretter, M.University of Munich, Federal Republic of GermanyauthorLichowski, F.Kiel University, Federal Republic of GermanyauthorBlackwell Scientific Publications for the Geological Society of Australia, Melbourne, AustraliapublisherdocumentHardcopyAustralian Journal of Earth Sciences50 (3)447-466ODP Leg 182 drilled two north-south transects in the western Great Australian Bight close to longitude 128 degrees E. These transects penetrated a remarkably thick section of uppermost Pliocene and Pleistocene carbonate sediments, which are separated from Miocene sections by a major hiatus. In the eastern transect, at sites 1129, 1131 and 1127,the Brunhes-Matuyama boundary (onset of C 1n) was found at 343 m, between 280 and 300 m, and at 343 m below the sea floor, respectively. In the western transect, at sites 1132 and 1130, it was found between 170 and 181 m, and at 200 m, respectively. Within the Brunhes chron, inclination and intensity fluctuations and correlations between susceptibility and standard delta (super 18) O records were used to give age-depth relations. These age relations from the palaeomagnetics are broadly consistent with the biostratigraphy and the delta (super 18) O results from Leg 182, but do not provide an entirely independent dataset. Rock magnetism stratigraphy at site 1131 revealed the principal bryozoan buildup to be at the time of the last glacial lowstand, as suggested by previous workers. At all sites the sedimentation rate increases from the basal unconformity up into the thick Upper Pleistocene section. In the western transect there appears to be a partial record of most of the Late Pliocene and Early Pleistocene chron boundaries (C 1r1n to C2An3n) in a condensed section, but in the eastern transect only the Jaramillo (C 1r1n) is observed.completedStratigraphyalgaeBrunhes ChronCenozoicForaminiferaGreat Australian BightIndian OceanInvertebrataJOIDESLeg 182magnetic susceptibilitymagnetostratigraphyMatuyama ChronmicrofossilsnannofossilsNeogeneOcean Drilling ProgramODP Site 1131paleoclimatologypaleomagnetismPlantaePleistocenePlioceneProtistaQuaternarysamplingTertiaryunconformitiesupper Cenozoicupper Quaternaryurn:org.iodp:exp:182urnlargerWorkCitationcampaignurn:org.iodp:exp:182:site:1131urnlargerWorkCitationstudyurn:org.iodp:exp:182urnlargerWorkCitationcampaignEnglishgeoscientificInformation123.3000135.5000-35.0000-31.4000Great Australian Bight