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Progress in Earth and Planetary Science
Fig. 7 | Progress in Earth and Planetary Science

Fig. 7

From: Possible climate preconditioning on submarine landslides along a convergent margin, Nankai Trough (NE Pacific)

Fig. 7

Core C0018 δ18O profile as a function of age based on tephrochronology and the LR04 stack (Lisiecki and Raymo 2005) before and after matching. The dataset from Bassinot et al. (1994) is shown in black. The gray arrows between the two curves indicate the timing of the matching points (X1–X4). The pink dotted lines indicate the dated tephras used as time markers for the correlation. Green arrows indicate MTDs. MIS stages are from Bassinot et al. (1994)

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