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The floating dendrochronological sequence of pine wood from Józefowo, N. Poland was expected to cover the ∼660 BC radiocarbon ( 14 C) excursion. The sequence was radiocarbon dated using the OxCal wiggle matching procedure and the IntCal20 calibration curve. 14 C concentrations were measured in one-year α-cellulose samples from around 660 BC. The published data on the ∼660 BC 14 C excursion from Grabie, Poland were used to absolute date the Józefowo chronology with 1-year accuracy. The results confirm the occurrence of a rapid increase in Δ 14 C in 664/663 BC and its potential to be used as a fixing point for floating dendrochronological sequences.
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Wiktorowski et al. (2024) studied this question.
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