The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …

A major puzzle of paleoclimatology is why, after a long interval of cooling climate, each late
Quaternary ice age ended with a relatively short warming leg called a termination. We here …

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 …

Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding
mechanisms of global climate change and associated sea-level fluctuations in the past …

Millennial-scale climate oscillations of the last ice age registered in Greenland and Antarctic
ice cores did not always vary in unison. A striking example is that the strongest Antarctic …

Abstract Reconstructing Northern Hemisphere ice-sheet oscillations and meltwater routing
to the ocean is important to better understand the mechanisms behind abrupt climate …

The British Palaeolithic provides the first academic synthesis of the entire British
Palaeolithic, from the earliest occupation (currently understood to be around 980,000 years …

Abstract The Middle and Late Pleistocene glaciations of northern Eurasia had a great impact
on the evolution of the modern drainage system. This paper presents a review and synthesis …

Deposits from three Pleistocene glaciations are found in north Germany. In most parts of
north Germany, the oldest glaciation, the Elsterian, reached furthest south. Only in the west …

The evolution and dynamics of the last British–Irish Ice Sheet (BIIS) have hitherto largely
been reconstructed from onshore and shallow marine glacial geological and …