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Dryad

Late Holocene tundra fires and linkages to climate and vegetation in northern Alaska

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Jun 24, 2025 version files 62.56 KB

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Abstract

Charcoal particles in lake-sediments can reveal past fires and linkages to climate and vegetation change. We use analyses of charcoal accumulation rates from two lakes (Lake I4 and Kirk Lake) on the Alaskan North Slope to reconstruct past fire activity, and charcoal morphology to identify changes in fuel sources. This dataset contains 1) chronological data for both lake-sediment cores used to construct age-depth models (Pb-210 and radiocarbon), 2) magnetic susceptibility measurements for both cores, 3) macroscopic charcoal particle counts for both sites at three size fractions (90-125µm, 125-250µm, and >250µm), and 4) charcoal morphology (classes defined in associated Arctic Science publication).