The only glaciers existing today in the Iberian Peninsula are small features located in the
Pyrenees, though their number and extension has undergone significant changes over the …

Abstract The Last Glacial Termination is marked by changing environmental conditions
affected by abrupt and rapid climate oscillations, such as Heinrich Stadial 1 (HS1), which is …

Heinrich Stadials significantly affected tropical precipitation through changes in the
interhemispheric temperature gradient as a result of abrupt cooling in the North Atlantic …

Rapid changes in ocean circulation and climate have been observed in marine-sediment
and ice cores over the last glacial period and deglaciation, highlighting the non-linear …

The main objective of this research is to improve knowledge of the deglaciation stages in
Sierra Nevada (southern Spain) by applying 36 Cl cosmogenic exposure dating to 28 …

Both hydroclimate proxies and modeling studies alike present compelling evidence for
abundant precipitation in southwestern North America and Europe at the Last Glacial …

We review the evolution of glaciers in the Iberian Mountains during the Younger Dryas (12.9–
11.7 ka, following the chronology of Greenland Stadial 1–GS1) and compare with available …

Abstract Comparison of selected, well-dated, lacustrine, speleothem and terrestrial pollen
records spanning the Holocene onset and the Early Holocene (ca. 11.7–8 cal kyrs BP) in the …

Quantitative continental climate reconstructions covering the last glacial cycle from the
Iberian Peninsula are scarce. In order to fill this gap, we obtained for the first time a high …

The spatial distribution and dating of archaeological sites suggest a poor occupation of
southern Iberia by hunter-gatherers after the Last Glacial Maximum (LGM) and during …