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dc.contributor.authorMangerud, Janeng
dc.contributor.authorLøvlie, Reidareng
dc.contributor.authorGulliksen, Steinareng
dc.contributor.authorHufthammer, Anne Karineng
dc.contributor.authorLarsen, Eiliveng
dc.contributor.authorValen, Vidareng
dc.date.accessioned2004-07-29T12:36:36Z
dc.date.accessioned2004-08-03T12:57:58Z
dc.date.accessioned2004-08-26T11:58:29Z
dc.date.available2004-07-29T12:36:36Z
dc.date.available2004-08-03T12:57:58Z
dc.date.available2004-08-26T11:58:29Z
dc.date.issued2003eng
dc.identifier.citationQuaternary Research 59(2): 213-222en
dc.identifier.issn0033-5894eng
dc.identifier.urihttp://hdl.handle.net/1956/405
dc.description.abstractTwo paleomagnetic excursions, the Skjong correlated with the Laschamp (about 41,000 GISP2 yr B.P.) and the Valderhaug correlated with the Mono Lake (about 34,000 GISP2 yr B.P.), have been identified in stratigraphic superposition in laminated clay deposited in ice-dammed lakes in three large caves in western Norway. During both periods the margin of the Scandinavian Ice Sheet advanced and reached the continental shelf beyond the outermost coastline. The mild, 4000-yr-long Ålesund interstade, when the coast and probably much of the hinterland were ice-free, separated the two glacial advances. The two paleomagnetic excursions have also been indirectly identified as increased fluxes of 36Cl and 10Be in the GRIP ice core, Greenland. This article presents a correlation between ice-margin fluctuations of the Scandinavian Ice Sheet and the stratigraphy of GRIP/GISP cores, using the paleomagnetic excursions and the 36Cl and 10Be peaks and thus circumventing the application of different dates or time scales. Some of the fluctuations of the Scandinavian Ice Sheet were of the "Allerød/Younger Dryas type" in the sense that its margin retreated during mild interstades on Greenland and readvanced during cold stades. However, some fluctuations were apparently not in phase with the Greenland climate.en
dc.format.extent42410 byteseng
dc.format.extent688283 byteseng
dc.format.extent166 byteseng
dc.format.mimetypetext/plaineng
dc.format.mimetypeapplication/pdfeng
dc.format.mimetypetext/plaineng
dc.language.isoengeng
dc.publisherElseviereng
dc.subjectScandinavian Ice Sheet fluctuationseng
dc.subjectÅlesund interstadeeng
dc.subjectLaschamp excursioneng
dc.subjectMono Lake excursioneng
dc.subjectDansgaard–Oeschger oscillationseng
dc.titlePaleomagnetic correlations between scandinavian ice-sheet fluctuations and greenland dansgaard–oeschger events, 45,000–25,000 yr B.P.eng
dc.typeJournal articleeng
dc.typePeer reviewedeng
dc.rights.holderElsevier Scienceeng
bora.peerreviewedPeer reviewedeng
bibo.doihttp://dx.doi.org/10.1016/S0033-5894(03)00010-3eng
dc.identifier.doihttp://dx.doi.org/10.1016/S0033-5894(03)00010-3


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