Combined optically stimulated luminescence and radiocarbon dating of aeolian dunes in Arctic Sweden

Abstract Multiple parabolic sand dune fields formed in Arctic Sweden after the last deglaciation, facilitated by an abundance of loose glaciofluvial sediment, limited vegetation cover and strong winds. Following initial stabilisation, these dunes underwent repeated reworking after fire events, as ev...

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Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Oehler, Salome, Stevens, Thomas, Kolb, Thomas, Possnert, Göran, Fuchs, Markus
Other Authors: Swedish Foundation for International Cooperation in Research and Higher Education, National Natural Science Foundation of China
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
Arctic
Jorggástat
Fennoscandia
Permafrost and Periglacial Processes
Online Access:http://dx.doi.org/10.1002/ppp.2216
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.2216
Description
Summary:Abstract Multiple parabolic sand dune fields formed in Arctic Sweden after the last deglaciation, facilitated by an abundance of loose glaciofluvial sediment, limited vegetation cover and strong winds. Following initial stabilisation, these dunes underwent repeated reworking after fire events, as evidenced by the presence of buried soils, charcoal layers and redeposited sands in the dune stratigraphy. These reworking events may be driven by wider climate forcing; however, to date, no chronological framework exists for this activity in Sweden. As such, here, we apply quartz optically stimulated luminescence (OSL) dating of Arctic Swedish sand dunes using two dunes at the sites of Vastakielinen and Jorggástat. Resultant double‐SAR (single aliquot regenerative dose) quartz OSL ages are in good agreement with independent ages provided by 14 C dating of charcoal fragments recovered from charcoal layers within the dunes, and we conclude that the chosen protocol is generally well suited for dating aeolian reworking of dune sediments in Arctic Sweden. While feldspar contamination limits precise age assignment for initial dune movement, our results nonetheless suggest repeated and long‐lasting aeolian activity in Arctic Sweden throughout the Holocene and, although there are differences in detail, further suggest some general trends in terms of dune stability and reworking over Arctic Fennoscandia.

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