Figure 5
From: Arctic cryosphere and Milankovitch forcing of Great Basin paleoclimate

Great Basin links to the Arctic over the Holocene. Comparison of (A) unfiltered Leviathan δ18Oivc and (B) insolation, (C) fossil tree radiocarbon dates at the Russian treeline32, (D) pollen-based summer temperature anomalies in the Western Canadian Arctic31, (E) and melt layer percentage in the Agassiz ice cap30 shows an orbital-scale control on Holocene Arctic and Great Basin paleotemperature. YD indicates the Younger Dryas chronozone.