Table 1

Coincidence of spectral lines in several records.

Period window 10Be concentr. 14C production φ Torque

85−89 86 88 88 86
103−106 104 105 105 104
146−151 148 150 150 147
206−210 207 209 209 209
503−515 504 512 508 504

Notes. The first column shows the chosen narrow windows for the five spectral lines observed in Fig. 5. Within the chosen windows all records of 10Be from the GRIP ice core (Vonmoos et al. 2006), 14C from tree rings (Reimer et al. 2009) and the φ record (Steinhilber et al. 2012) show the same spectral lines.

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