Figure 3

INTIMATE event stratigraphy plotted along the NGRIP and GISP2 δ¹⁸O and Ca²⁺ ice core records from Greenland³⁴; selected dung fungal spores (Sporomiella, HdV55a) indicating the presence of large bodied grazers in the Kokad pollen profile¹⁸; calibrated BP intervals of presence for selected mega- and microfauna elements in the Carpathian Basin dated within the scope of this study; summary pollen diagrams from two sites (Lake St Anne—950 m a. s. l.¹³ and Kokad Mire—112 m a. s. l.¹⁸) showing the cumulative percentage of total tree, shrub and herb pollen types and elm (Ulmus) pollen, and separate non-cumulative relative frequency curves for major herb pollen types (Chenopodium-type, Artemisia, Poaceae, Cyperaceae), palynological richness, microcharcoal influx, macrocharcoal inferred fire frequency curves, peak fire magnitudes and fire events (red crosses) from the same pollen sites. The methodology of macrocharcoal analyses is described in the Supplementary Material.