five

(Table S1) Age models of sediment cores OCE326-GGC5, OCE326-GGC6 and EN120-GGC1

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All three cores were matched using magnetic susceptibility and age models were applied using OCE326-GGC5 radiocarbon ages (Gherdardi et al., 2005, doi:10.1016/j.epsl.2005.09.061).
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