The Quaternary Period (the last 2.58 Ma) was characterized by the waxing and waning of large ice sheets in the Northern Hemisphere. Using sediment sequences from the Iberian Margin, we demonstrate tha...

Ice sheets can be extremely sensitive, or remarkably resilient, to environmental perturbations. Reconstructions of past ice sheet variability help identify what controls their stability and how they m...

Large benthic oxygen isotope fluctuations in the Oligocene Southern Ocean primarily represent deep water temperature changes, suggesting the Antarctic ice sheet volume was relatively stable, according...

PyAnalySeries Reimagined: A Legacy Tool Reborn. Contribute to PaleoIPSL/PyAnalySeries development by creating an account on GitHub.

High fidelity benthic foraminifera oxygen isotope records reveal that variations in Earth’s orbit are the primary pacemaker of change in early Antarctic ice ages and caused these ice ages to sometimes...