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dc.contributor.authorAndersen, Jane Lund
dc.contributor.authorMargreth, Annina
dc.contributor.authorFredin, Ola
dc.contributor.authorLinge, Henriette
dc.contributor.authorGoodfellow, Bradley W.
dc.contributor.authorFaust, Johan Christoph
dc.contributor.authorKnies, Jochen
dc.contributor.authorSolbakk, Terje
dc.contributor.authorBrook, Edward J.
dc.contributor.authorScheiber, Thomas
dc.contributor.authorvan der Lelij, Roelant
dc.contributor.authorBurki, Valentin Josef
dc.contributor.authorRubensdotter, Brita Lena Eleonor Fredin
dc.contributor.authorHimmler, Tobias
dc.contributor.authorYesilyurt, Serdar
dc.contributor.authorChristl, Marcus
dc.contributor.authorVockenhuber, Christof
dc.contributor.authorAkcar, Naki
dc.date.accessioned2022-08-12T12:20:45Z
dc.date.available2022-08-12T12:20:45Z
dc.date.created2021-11-05T11:42:59Z
dc.date.issued2022
dc.identifier.issn0169-555X
dc.identifier.urihttps://hdl.handle.net/11250/3011656
dc.description.abstractQuantifying bedrock weathering rates under diverse climate conditions is essential to understanding timescales of landscape evolution. Yet, weathering rates are often difficult to constrain, and associating a weathered landform to a specific formative environment can be complicated by overprinting of successive processes and temporally varying climate. In this study, we investigate three sites between 59°N and 69°N along the Norwegian coast that display grussic saprolite, tafoni, and linear weathering grooves on diverse lithologies. These weathering phenomena have been invoked as examples of geomorphic archives predating Quaternary glaciations and consequently as indicators of minimal glacial erosion. Here we apply cosmogenic nuclide chronometry to assess the recent erosional history. Our results demonstrate that all three sites experienced sufficient erosion to remove most cosmogenic nuclides formed prior to the Last Glacial Maximum. This finding is inconsistent with preservation of surficial (<1–2 m) weathered landforms under non-erosive ice during the last glacial period, while simultaneously demonstrating that post-glacial weathering and erosion rates can be locally rapid (4–10 cm kyr−1) in cold temperate to subarctic coastal locations.en_US
dc.language.isoengen_US
dc.relation.urihttps://www.sciencedirect.com/science/article/pii/S0169555X21004116
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleRapid post-glacial bedrock weathering in coastal Norwayen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2021 The Author(s)en_US
dc.source.articlenumber108003en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1016/j.geomorph.2021.108003
dc.identifier.cristin1951725
dc.source.journalGeomorphologyen_US
dc.relation.projectNorges forskningsråd: 319849en_US
dc.identifier.citationGeomorphology. 2022, 397, 108003.en_US
dc.source.volume397en_US


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