Although detailed age models exist for some marine sediment records of the last glacial
cycle (0–150 ka), age models for many cores rely on the stratigraphic correlation of benthic …

Benthic δ18O is often used as a stratigraphic tool to place marine records on a common age
model and as a proxy for the timing of ice volume/sea level change. However, Skinner and …

We present a 5.3‐Myr stack (the “LR04” stack) of benthic δ18O records from 57 globally
distributed sites aligned by an automated graphic correlation algorithm. This is the first …

Benthic δ18O changes are often assumed to be globally synchronous, but studies
comparing 2–9 radiocarbon‐dated records over the most recent deglaciation (Termination …

Late Pleistocene sea level has been reconstructed from ocean sediment core data using a
wide variety of proxies and models. However, the accuracy of individual reconstructions is …

High-resolution seawater δ 18 O records, derived from coupled Mg/Ca and benthic δ 18 O
analyses, can be used to evaluate how global ice volume changed during the mid …

Based on benthic foraminiferal δ18O from ODP Site 1143, a 5-Myr astronomical timescale
for the West Pacific Plio–Pleistocene was established using an automatic orbital tuning …

Unraveling the dynamics of the Northern Hemisphere glaciation (NHG) in the Pliocene is a
key step toward a quantitative theory of the climate transition from a greenhouse to an …

We review the various methods which have been applied to estimate the change of
seawater δ18O (δw) between the Last Glacial Maximum (LGM) and the Holocene. The most …

Understanding the sensitivity of the polar ice caps to a modest global warming (2–3° C
above preindustrial) is of paramount importance if we are to accurately predict future sea …