Late Quaternary productivity changes from offshore Southeastern Australia: A biomarker approach

► Productivity in offshore SE Australia shows strong variations for the last ~ 135 ka. ► Deglacial minima in planktonic foram δ13C suggests input of Southern Ocean waters. ► TOC and haptophyte productivity are likely related to strong westerly winds. ► Proboscia diatom productivity is likely related to silica transport from SO waters.