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. 2004 Apr 19;101(17):6341–6345. doi: 10.1073/pnas.0400323101

Fig. 2.

Fig. 2.

Interval over which the correlation was calculated, with hashing to indicate Siple Dome volcanic events (Lower) and GISP2 DO cold events (Upper). For clarity, a few of the weakest volcanic events are not indicated. The stadial near 67 ka has been associated with the Toba supereruption (28).