10Be dating of Younger Dryas Salpausselkä I formation in Finland

• Published in: Boreas
• Main Authors: TSCHUDI, SILVIO, IVY‐OCHS, SUSAN, SCHLÜCHTER, CHRISTIAN, KUBIK, PETER, RAINIO, HEIKKI
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2000
• Subjects: Greenland; Lahti; Fennoscandian; GISP; GRIP; ice core
• Online Access: http://dx.doi.org/10.1111/j.1502-3885.2000.tb01211.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.2000.tb01211.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.2000.tb01211.x

Boulders of the Younger Dryas Salpausselkä I (Ss I) formation west of Lahti, southern Finland, were sampled for surface exposure dating. The 10 Be concentrations, determined by accelerator mass spectrometry, yield minimum exposure ages of 11 930 ± 950, 11 220 ± 890, 11 050 ± 910 and 11 540 ± 990 years, using recently published production rates scaled for latitude and elevation. This includes a correction to the production rate resulting from postglacial uplift of the Fennoscandian lithosphere (i.e. changing elevation) during the time of exposure. The error‐weighted mean exposure age of 11 420 ± 470 years of the analysed boulders agrees with previous varve dates of Ss I, which range from 11 680 to 11 430 calendar years BP. However, erosion has to be taken into account as a process affecting rock surfaces and therefore influencing exposure ages. Available information suggests an erosion rate of 5 mm/kyr, which increases the error‐weighted mean exposure age to a value of 11 610 ± 470 years. Within the errors, the formation of Ss I in the Vesala area west of Lahti falls into the Younger Dryas time bracket, as defined by the GRIP and GISP 2 ice core (Greenland).