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Palynology of Neogene slope and rise deposits from ODP sites 1165 and 1167, East Antarctica

Macphail, Michael; Truswell, Elizabeth

Description

Sites 1165 and 1167 were drilled on the continental slope and rise seaward of Prydz Bay, East Antarctica. The sediments penetrated are glacigene and independently dated as Neogene age (early Miocene and younger) using diatoms, radiolarians, nannofossils,

dc.contributor.authorMacphail, Michael
dc.contributor.authorTruswell, Elizabeth
dc.date.accessioned2015-12-13T22:50:41Z
dc.date.available2015-12-13T22:50:41Z
dc.identifier.issn0884-5891
dc.identifier.urihttp://hdl.handle.net/1885/80906
dc.description.abstractSites 1165 and 1167 were drilled on the continental slope and rise seaward of Prydz Bay, East Antarctica. The sediments penetrated are glacigene and independently dated as Neogene age (early Miocene and younger) using diatoms, radiolarians, nannofossils,
dc.publisherTexas A&M University
dc.sourceProceedings of the Ocean Drilling Program, Scientific Results
dc.subjectKeywords: Bacillariophyta; Batiacasphaera; Cymatiosphaera; Dinophyceae; Fagus; Gymnospermae; Nothofagus; Radiolaria (protozoans)
dc.titlePalynology of Neogene slope and rise deposits from ODP sites 1165 and 1167, East Antarctica
dc.typeJournal article
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.citationvolume188
dc.date.issued2004
local.identifier.absfor060206 - Palaeoecology
local.identifier.ariespublicationMigratedxPub9211
local.type.statusPublished Version
local.contributor.affiliationMacphail, Michael, College of Asia and the Pacific, ANU
local.contributor.affiliationTruswell, Elizabeth, College of Physical and Mathematical Sciences, ANU
local.bibliographicCitation.startpage1
local.bibliographicCitation.lastpage20
dc.date.updated2016-02-24T09:49:53Z
local.identifier.scopusID2-s2.0-79953275168
CollectionsANU Research Publications

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