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

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Figure

Fig. 3 Correlation of seismic data with core C0018. Data from previous studies are shown, including lithology and dating of C0018 based onmagnetostratigraphy, nannofossil biostratigraphy, and tephrochronology (Ss-Az and As-Pnk) from lithological unit U1a (
Fig. 4 Examples of sedimentological features of the hemipelagic sediment (a) and of various parts of the MTDs (such as mudclasts in b, d and e;turbidites in c and mixed sediments in f)
Table 2 Radiocarbon ages obtained for foraminiferas (Globigerina inflata). Calibration was performed with the “calibrate” function ofthe clam code (Blaauw 2010) from the open-source statistical software “R” using the marine calibration curve Marine13.14C (
Table 3 Tephra ages used as time references for δ18O isotope stratigraphy. The estimated age, method of age determination, andreferences are given for each tephra age
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