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dc.rights.licenseopenen_US
dc.contributor.authorBOES, Evelien
dc.contributor.authorVAN DAELE, Maarten
dc.contributor.authorMOERNAUT, Jasper
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
dc.contributor.authorJENSEN, Britta J. L.
dc.contributor.authorPRAET, Nore
dc.contributor.authorKAUFMAN, Darrell
dc.contributor.authorHAEUSSLER, Peter
dc.contributor.authorLOSO, Michael G.
dc.contributor.authorDE BATIST, Marc
dc.date.accessioned2024-04-10T12:32:34Z
dc.date.available2024-04-10T12:32:34Z
dc.date.issued2017-11-22
dc.identifier.issn0016-7606en_US
dc.identifier.uriorcid:0000-0001-9134-7170:10.1130/b31792.1
dc.identifier.urioai:crossref.org:10.1130/b31792.1
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/197418
dc.description.abstractEnThe sediments stored in the large, deep proglacial lakes of south-central Alaska are largely unstudied. We analyzed sediments in 20 cores, up to 160 cm long, from Eklutna, Kenai, and Skilak Lakes, using a combination of repeated lamination counting, radionuclide dating, event stratigraphy, and tephrochronology. We show that the characteristically rhythmic layers were deposited annually. Most of these glacial varves consist of one coarse-grained base and a fine-grained top, but varves composed of multiple coarse-grained turbidite pulses are common too. They are likely related to successive episodes of high sediment discharge during flooding, and they become more frequent in all three lakes, along with increased sedimentation rates, during the nineteenth century late phase of the Little Ice Age. These flood turbidites were generated by rain events and intense melting of snow and ice. Other (mega) turbidites are a result of earthquake-triggered slope collapses (e.g., A.D. 1964). Some event layers are present in all three lakes. In addition, the annual time series of varve thickness (normalized annual sedimentation rate) are significantly correlated among the three lakes (ρ > 0.27; p < 0.001). Differences between the varve thickness records can be attributed partly to the dam construction at Eklutna Lake and outbursts from an ice-dammed lake at Skilak Lake. Geomorphologic differences among the catchments result in further differences in sedimentation patterns in the three lakes.
dc.language.isoENen_US
dc.sourceorcid
dc.sourcecrossref
dc.title.enVarve formation during the past three centuries in three large proglacial lakes in south-central Alaska
dc.typeArticle de revueen_US
dc.identifier.doi10.1130/b31792.1en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalGeological Society of America Bulletinen_US
bordeaux.page757-774en_US
bordeaux.volume130en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue5-6en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamSEDIMen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04540826
hal.version1
hal.date.transferred2024-04-10T12:32:37Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&amp;rft_val_fmt=info:ofi/fmt:kev:mtx:journal&amp;rft.jtitle=Geological%20Society%20of%20America%20Bulletin&amp;rft.date=2017-11-22&amp;rft.volume=130&amp;rft.issue=5-6&amp;rft.spage=757-774&amp;rft.epage=757-774&amp;rft.eissn=0016-7606&amp;rft.issn=0016-7606&amp;rft.au=BOES,%20Evelien&amp;VAN%20DAELE,%20Maarten&amp;MOERNAUT,%20Jasper&amp;SCHMIDT,%20Sabine&amp;JENSEN,%20Britta%20J.%20L.&amp;rft.genre=article


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