Deep-sea pollen records from the Western European margin show that during the Last
Glacial period (115-27 ka), regional vegetation oscillated between steppe and open forest in …

One of the most important problems in glacial geomorphology is the disagreement regarding
the dates of glacial advances. During the Last Glacial Maximum (LGM,~ 29 to 19 ka), the …

The response of European precipitation variability to climate change is still poorly
understood. Here we present a high-resolution speleothem record of Eastern Central …

Quantifying the timing and extent of Quaternary mountain glaciations can help us in
understanding the cause of ice-age cycles. As such, impressive achievements have been …

The accelerating flux of glacial meltwater to the oceans due to global warming is a potential
trigger for future climate disturbance. Past disruption of Atlantic Ocean circulation, driven by …

Radiocarbon dating provides a key chronological framework for studying past environmental
changes. Raw radiocarbon ages measured in samples must be converted to calendar ages …

Pleistocene glacial activity was a major influence on runoff and sediment supply in many
river systems across the Mediterranean. The geomorphological impacts of changes in …

The area of Prados del Cervunal (PC) is an intra-morainic topographic depression located at
1800 m asl in the divide or interfluve between Garganta de Gredos and Garganta del Pinar …

Large glaciers and ice caps formed in the Mediterranean mountains during the cold stages
of the Pleistocene and some small glaciers remain today. Here we review 157 outputs that …

The chronology of the late Pleistocene glaciation in the Massif Central, France, is not well
documented and there are divergent hypotheses regarding the timing of glacial events in …