Benthic foraminiferal stable isotopes, planktonic foraminiferal biostratigraphy and seismic profiles for IODP Site 356-U1463
Determining the age of marine sediments is essential to reconstruct past changes in oceanography and climate. The oxygen isotopes of benthic foraminifera record long-term changes in global ice volume and deep-water temperature, and are commonly used to construct age models. However, continental marg...
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