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The frequency of lamination in the sediments of Lake Barrine, tropical north-east Australia, during the last five millennia

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dc.contributor.authorWalker, Donald
dc.date.accessioned2015-12-10T23:17:54Z
dc.date.issued2011
dc.date.updated2016-02-24T08:09:05Z
dc.description.abstractAt Lake Barrine (17°15'S, 145°38'E, 721. m a.s.l.) under water > 55. m deep, the uppermost sediment is composed of alternating detritus-poor and detritus-rich laminae. The former are interpreted as the continuous sedimentation (mostly plankton) from the
dc.identifier.issn0031-0182
dc.identifier.urihttp://hdl.handle.net/1885/65401
dc.publisherElsevier
dc.sourcePalaeogeography, Palaeoclimatology, Palaeoecology
dc.subjectKeywords: geoaccumulation; Holocene; lacustrine deposit; lamination; paleoclimate; radiocarbon dating; wind direction; Australia; Lake Barrine; Queensland; Placida Australia; Holocene; Lake Barrine; Laminations; Sediments; Tropics
dc.titleThe frequency of lamination in the sediments of Lake Barrine, tropical north-east Australia, during the last five millennia
dc.typeJournal article
local.bibliographicCitation.issue1-2
local.bibliographicCitation.lastpage226
local.bibliographicCitation.startpage214
local.contributor.affiliationWalker, Donald, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidWalker, Donald, a102754
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor060206 - Palaeoecology
local.identifier.absfor040605 - Palaeoclimatology
local.identifier.absfor040310 - Sedimentology
local.identifier.absseo960304 - Climate Variability (excl. Social Impacts)
local.identifier.absseo970105 - Expanding Knowledge in the Environmental Sciences
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationf2965xPUB1100
local.identifier.citationvolume299
local.identifier.doi10.1016/j.palaeo.2010.11.003
local.identifier.scopusID2-s2.0-78650593727
local.type.statusPublished Version

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