Planktonic foraminifera δ18O and concentrations of major and trace elements from IODP Hole U1432C
Published: 22 December 2023| Version 1 | DOI: 10.17632/sk43xgzfdk.1
Contributors:
, , , Felipe Stanchak, Description
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.
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Institutions
- Universidade de Sao Paulo
- Universidade Federal do Parana
Categories
Geochemistry, Paleoceanography, Paleoclimate Proxy, Marine Geology, Paleoclimatology