This dataset is about: Stable oxygen isotopic ratios of benthic foraminifera of IODP Site 339-U1389. Please consult parent dataset @ https://doi.org/10.1594/PANGAEA.871499 for more information.
Determining the timing and amplitude of tropical sea surface temperature (SST) change is an important part of solving the puzzle of the Plio-Pleistocene ice ages. Alkenone-based tropical SST records f
Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Peninsula and recorded changes in glacial volume and thermal regime over the last ca. 15 m.y. At Ocean
