Abstract
Astronomically tuned high-resolution climatic proxy records across marine oxygen isotope stage 100 (MIS100) from the
Italian Monte San Nicola section and ODP Leg 160 Hole 967A are presented. These records reveal a complex pattern of climate
fluctuations on both Milankovitch and sub-Milankovitch timescales that oppose or reinforce one another. Planktonic and
benthic foraminiferal
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