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dc.contributor.authorP. Hesse, Paulen_US
dc.contributor.authorMcTainsh, Granten_US
dc.contributor.editorJim Rose, P U Clark, Rainer Gruenen_US
dc.date.accessioned2017-05-03T11:22:07Z
dc.date.available2017-05-03T11:22:07Z
dc.date.issued2003en_US
dc.date.modified2009-01-12T06:20:43Z
dc.identifier.issn02773791en_US
dc.identifier.doi10.1016/S0277-3791(03)00164-1en_AU
dc.identifier.urihttp://hdl.handle.net/10072/5971
dc.description.abstractA detailed record of the deglaciation history of the penultimate glacial to interglacial transition is given, mainly based on the stable isotopes of calcium carbonate-containing lake sediments in a glacially excavated depression below the city of Amsterdam. Initially, this depression, the Amsterdam Basin, formed part of a lake covering the western and central part of the Netherlands and extending for an unknown distance into the present North Sea. Annual layer counting shows that the lake drained after about a millennium, leaving shallow pools in the remaining depressions. The latter changed again into larger and deeper lakes including the Holland Lake during the rise of sea level in the early Eemian. Oxygen isotope values of the early lake sediments indicate an interglacial summer climate, but the nearness of dead-ice fields caused severe winters. The isotope record is furthermore characterized by the influx of large amounts of isotopically light water supplied by the river Rhine. A change to much colder conditions occurred simultaneously with the draining of the Holland Lake, as appears from oxygen isotope values and the sudden increase in non-arboreal pollen. This interval is correlated with the Kattegat Stadial and the sea-level standstill of Aladdins Cave on the Huon Peninsula of New Guinea. A short climate wiggle occurs at the end of this interval. The onset of the Eemian is marked by a rapid warming of 5àwhich extends into local pollen-zone E3. Provided that our correlation of this cold interval with the sea-level standstill of Aladdins Cave is correct, the time interval between the earliest lake sediments in the Amsterdam Basin and the Eemian highstand took about 5-6 millennia.en_US
dc.description.peerreviewedYesen_US
dc.description.publicationstatusYesen_AU
dc.languageEnglishen_US
dc.language.isoen_AU
dc.publisherPergamonen_US
dc.publisher.placeUnited Kingdomen_US
dc.publisher.urihttp://www.elsevier.com/wps/find/journaldescription.cws_home/636/description#descriptionen_AU
dc.relation.ispartofpagefrom2007en_US
dc.relation.ispartofpageto2035en_US
dc.relation.ispartofedition2003en_US
dc.relation.ispartofissue18/19en_US
dc.relation.ispartofjournalQuaternary Science Reviewsen_US
dc.relation.ispartofvolume22en_US
dc.subject.fieldofresearchcode260114en_US
dc.titleAustralian dust deposits: modern processes and the Quaternary recorden_US
dc.typeJournal articleen_US
dc.type.descriptionC1 - Peer Reviewed (HERDC)en_US
dc.type.codeC - Journal Articlesen_US
gro.rights.copyrightCopyright 2003 Elsevier : Reproduced in accordance with the copyright policy of the publisher : This journal is available online - use hypertext links.en_AU
gro.date.issued2003
gro.hasfulltextNo Full Text


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