Site U1462

Site U1506

“…The needle probe was used on whole-round sections from Cores 371-U1506A-1R through 25R, and the puck method was used on Cores 26R through 28R. Thermal conductivity data show a gradual and increasing trend with depth from 1.1 to 1.4 W/(m·K) over the uppermost ~250 m, consistent with expected values for calcareous ooze and chalk (Gallagher et al, 2017).…”

Site U1464

“…MS was measured during downhole logging with the triple combo in Hole U1464C. Similar to what was observed during downhole logging at IODP Sites U1461-U1463, the wireline MS measurements were affected by temperature (see Downhole measurements in the Site U1461 chapter, Downhole measurements in the Site U1462 chapter, and Downhole measurements in the Site U1463 chapter [Gallagher et al, 2017b[Gallagher et al, , 2017c[Gallagher et al, , 2017d). This resulted in wireline MS measurements that were not comparable to MS data measured on cores.…”

Expedition 356 summary

“…Biostratigraphic zone boundary ages are shown. Age-depth model was produced from select biostratigraphic datums (see Table T7 in the Site U1462 chapter [Gallagher et al, 2017f ]) (solid circles = calcareous nannofossil, open circles = planktonic foraminifer). Sedimentation rates are calculated separately for planktonic foraminiferal (blue dashed line) and calcareous nannofossil (green line) datums and assume a linear sedimentation rate between datums.…”