georefid:2004-084089SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1130/G20783.1<gco:CharacterString>Canterbury Drifts at Ocean Drilling Program Site 1119, New Zealand; climatic modulation of Southwest Pacific intermediate water flows since 3.9 Ma</gco:CharacterString>2004-01-01publicationgeorefid:2004-084089doi:10.1130/G20783.1Carter, R. M.James Cook University, Marine Geophysical Laboratory, Townsville, Queensl., AustraliaauthorFulthorpe, C. S.University of Texas at Austin, United StatesauthorLu, H.authorGeological Society of America (GSA), Boulder, CO, United StatespublisherdocumentHardcopyGeology (Boulder)32 (11)1005-1008We provide a record of variations in southwest Pacific Ocean intermediate water flow that shows a strong correlation between periods of vigorous flow and warm climate phases. Ocean Drilling Program Site 1119, located at 395 m water depth on the upper continental slope east of New Zealand, penetrated 514 m of silts and silty clays (glacial deposits) punctuated by muds and episodic 0.02-1.2-m-thick terrigenous sands (interglacial deposits). The natural gamma-ray record reflects the waxing and waning of the South Island ice cap since 3.91 Ma. Below 86.19 m composite depth, the succession comprises drift sediments deposited from north-flowing intermediate Subantarctic Mode Water (SAMW, approximately 250-800 m depth) and Antarctic Intermediate Water ( approximately 800-1100 m depth). A change from the deposition of large, low-energy drifts on the middle slope to smaller, higher-energy drifts on the upper slope coincided with global climatic deterioration that occurred after ca. 3.25 Ma. This change marks an upward expansion of intermediate cold waters, perhaps caused by the inception of the Subantarctic Front and the consequent commencement of Southland Current-driven SAMW flow.completedStratigraphyApplied geophysicsAntarctic Intermediate WaterAustralasiaCanterbury DriftsCenozoicclastic sedimentsclayclimate changecontinental margin sedimentationcontinental slopecoresdepositional environmentdriftgeophysical methodsgeophysical surveysglacial environmentglaciomarine environmenthigh-resolution methodsinterglacial environmentLeg 181marine environmentmarine sedimentsmudmultichannel methodsNeogeneNew Zealandocean circulationOcean Drilling ProgramODP Site 1119Pacific Oceanpaleo-oceanographypaleocirculationpaleoclimatologyPlioceneQuaternarysedimentationsedimentsseismic methodsslope environmentSouth IslandSouth PacificSouthern OceanSouthwest PacificSubantarctic Mode WatersurveysTertiaryupper PlioceneWest Pacificurn:org.iodp:exp:181urnlargerWorkCitationcampaignurn:org.iodp:exp:181:site:1119urnlargerWorkCitationstudyurn:org.iodp:exp:181urnlargerWorkCitationcampaignEnglishgeoscientificInformation172.2336172.2336-44.4520-44.4520Includes 1 insert