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Late Quaternary palaeoceanography of the Circumpolar Deep Water from South Tasman Rise

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dc.contributor.authorMoy, Andrew D
dc.contributor.authorHoward, William Robert
dc.contributor.authorGagan, Michael
dc.date.accessioned2015-12-07T22:31:15Z
dc.date.issued2006
dc.date.updated2015-12-07T10:14:44Z
dc.description.abstractWe use sediment cores from the South Tasman Rise (STR) to reconstruct deepwater circulation in the southwest Pacific sector of the Southern Ocean. Sediment cores MD972106 (45° 09′ S, 146° 17′ E, 3310 m water depth) and GC34 (45° 06′ S, 147° 45�
dc.identifier.issn0267-8179
dc.identifier.urihttp://hdl.handle.net/1885/22693
dc.publisherWiley-VCH Verlag GMBH
dc.sourceJournal of Quaternary Science
dc.subjectKeywords: accelerator mass spectrometry; benthic foraminifera; carbon isotope; circumpolar current; deep water formation; paleoceanography; Quaternary; radiocarbon dating; stable isotope; Southern Ocean; Cibicidoides; Foraminifera Benthic foraminiferal stable isotopes; Circumpolar deep water; Deep-water circulation; Palaeoceanography; Southern Ocean
dc.titleLate Quaternary palaeoceanography of the Circumpolar Deep Water from South Tasman Rise
dc.typeJournal article
local.bibliographicCitation.issue7
local.bibliographicCitation.lastpage777
local.bibliographicCitation.startpage763
local.contributor.affiliationMoy, Andrew D, University of Tasmania
local.contributor.affiliationHoward, William Robert, University of Tasmania
local.contributor.affiliationGagan, Michael, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidGagan, Michael, u9203225
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor049999 - Earth Sciences not elsewhere classified
local.identifier.ariespublicationu3533991xPUB23
local.identifier.citationvolume21
local.identifier.doi10.1002/jqs.1067
local.identifier.scopusID2-s2.0-33750406173
local.type.statusPublished Version

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