The glacial-interglacial transitions of ice ages are associated with large, rapid changes in
climate, which potentially can be reconstructed from stratigraphic profiles of the chemical …

It has long been known that mountain glaciers and continental ice sheets around the globe
reached their respective maximum extent at different times during the last glacial cycle, often …

The Younger Dryas (YD) was a period of rapid climate cooling that occurred at the end of the
last glaciation. Here, we present the first palaeoglacier-derived reconstruction of YD …

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 …

Throughout the last cold stage, the North Atlantic region was punctuated by abrupt climate
shifts and atmospheric processes propagated their effects to adjacent continents. During …

While revolutionary to the geomorphic community, the application of terrestrial cosmogenic
nuclide (TCN) dating is complicated by geological uncertainties, which often lead to skewed …

Active periglacial processes are currently marginal in the Iberian Peninsula, spatially limited
to the highest mountain ranges. However, a wide variety of periglacial deposits and …

This paper summarizes the current state of knowledge about the millennial scale climate
variability characterizing Marine Isotope Stage 3 (MIS 3) in S-Europe and the Mediterranean …

In this paper we synthesize the research in glacial geomorphology and geochronology in
northern Spain, with special attention to the evidence of local glacier maximum extent earlier …

At the north-western limit of the Mediterranean basin, in the Mediterranean–Oceanic
transition zone, the multidisciplinary study of two palaeolakes: Villaseca and La Mata …