Sampling was conducted at TAMU ~3 months after the cruise. Samples of ~20 cm3 in volume were taken from Cores 167-1017E-1H through 3H in 3-cm intervals. These samples were immediately placed in k-packs, vacuum sealed, and double packed. Samples for X-ray radiography were taken separately as 20-cm-long thin slabs. The slab samples were taken continuously throughout cores using a plastic case of 20 × 2 × 0.7 cm in size and immediately sealed. These samples were sent to the University of Tokyo and stored in a refrigerator under 10°C. All the samples taken from Core 1H (197 samples) and every other sample from Core 2H (168 samples) were subject to inorganic geochemical analyses.
For X-ray diffraction (XRD), X-ray fluorescence (XRF), and carbon analyses, ~12 g of wet samples were washed and centrifuged twice with double distilled water to completely remove salts. The centrifuged samples were dried at 50°C for 24-48 hr, powdered with an agate mortar, and stored in glass tubes.
For grain-size analysis, the following three steps of chemical treatment, which are modified from the procedure of Rea and Janecek (1981), were applied to the samples to isolate the detrital component. Because the studied samples contain only trace amounts of siliceous bioclasts, an opal removal treatment was not conducted.
After this chemical leaching procedure, samples were kept wet to prevent aggregation. All the treated samples were introduced into the grain-size analyzer to prevent grain-size segregation during transfer.