Planktonic foraminifera δ18O and concentrations of major and trace elements from IODP Hole U1432C

We investigate the last 230 kyr terrigenous input changes to the northeast SCS deep-sea based geochemical properties of Hole U1432C (3829 m water depth) retrieved by the International Ocean Discovery Program (IODP) Expedition 349. The dataset includes δ18O stable isotope signal obtained from planktonic foraminifera (Globigerinoides ruber white > 150 µm) and elemental composition of the sediments.