A tephrostratigraphic investigation of the continuously varved Holocene Boreal lake Nautajärvi, Finland, provides precise age estimate for Lairg A/Hekla 5 eruption
: Carter‐Champion, Alice; Flowers, Katy; Ojala, Antti E.K.; Blockley, Simon; Lincoln, Paul; Zhang, Shuang; Manning, Christina; Puertas, Celia Martin
Publisher: Wiley
: HOBOKEN
: 2025
: Journal of Quaternary Science
: Journal of Quaternary Science
: J QUATERNARY SCI
: 18
: 0267-8179
: 1099-1417
DOI: https://doi.org/10.1002/jqs.70006
: https://doi.org/10.1002/jqs.70006
: https://research.utu.fi/converis/portal/detail/Publication/499594072
Numerous cryptotephra layers originating from Icelandic volcanoes and further afield have reached Northern Europe during the Holocene. Refining the precise timing and the relative frequency of local and distal eruptions requires well-resolved continuous sediment archives. Lake Nautajarvi is located in central-southern Finland (61 degrees 48 ' N, 24 degrees 41 ' E), and contains a continuous sequence of 9898 varves. Nautajarvi was isolated from the Baltic Sea basin at the Lake Ancylus phase similar to 9600 varve yr BP. We present a tephrostratigraphic record of Nautajarvi for targeted intervals within the Holocene, aiming to identify tephra from the largest eruptions, to enable an alignment with other varved lakes in Northern Europe containing tephra layers, like Diss Mere, Tiefer See and Meerfelder Maar. Geochemical analyses were produced for 26 peaks in tephra concentration, with five cryptotephra deposits corresponding to known eruptions from the mid and late Holocene. The far-travelled KS2 eruption from Ksudach caldera in Kamchatka is identified, enabling an alignment to Greenland, which is strengthened by the identification of the Hekla 4 tephra in Nautajarvi. Close to the KS2 deposition in Nautajarvi, a Hekla-type eruption correlating to the Lairg A/Hekla 5 is also identified-macroscale counting of the varves between the KS2 and Lairg A layers enables a constrained age estimate (7001 +/- 44 Cal yr BP) of the Lairg A eruption to be made. The widespread Glen Garry tephra was also identified within the Nautajarvi sequence, with an age estimate of 2088 +/- 21 varve yr BP. Finally, there is also a tentative correlation to the Suduroy tephra, with an older age estimate than from the sites in which it was originally identified (8459 +/- 84 varve yr BP). The remaining layers correspond to eruptions from more distal sources-several chemistries may correlate to mid-Holocene eruptions from North America (Mount Rainier, Aniakchak, Katmai), with one shard tentatively associated with Azorean chemistry. This record provides well-constrained age estimates for two key Holocene tephras (Glen Garry, Lairg A) and highlights the potential for far-travelled tephras from North America and Kamchatka to reach Northern Europe, emphasising the benefits of further tephra studies in Scandinavia. (c) 2025 The Author(s).Journal of Quaternary Science Published by John Wiley & Sons Ltd.
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This study was funded by the UKRI Medical Research Council through a Future Leaders Fellowship held by Celia Martin-Puertas, contributing to the research project DECADAL: Rethinking Palaeoclimatology for Society (MR/W009641/1). Antti Ojala was supported by Digital Waters Flagship (DIWA) (decision no. 359247) funded by the Research Council of Finland. The authors thank Saija Saarni and Emilia Kosonen, who helped with coring of Nautajaervi, as well as two anonymous reviewers, whose comments helped to improve the paper.
