Abstract The Little Ice Age (LIA) is known as one of the coldest stages of the Holocene. Most
records from the Northern Hemisphere show evidence of significantly colder conditions …

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 …

The relatively warm climate conditions prevailing today in the Mediterranean region limit
cold geomorphological processes only to the highest mountain environments. However …

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 …

Several stalagmite records have yielded important but discontinuous insights into northern
Iberian climate since the Last Glacial. Here we present the first continuous Iberian stalagmite …

Time and circumstances for the disappearance of Neanderthals and its relationship with the
advent of Modern Humans are not yet sufficiently resolved, especially in case of the Iberian …

Glaciers were common across the Mediterranean mountains during the Little Ice Age. In
parts of Turkey some glaciers were several kilometres longer than they are today, whilst in …

The aim of this research is to improve our current understanding of the deglaciation stages
in the southeastern Pyrenees and integrate it into reconstructions of the long‐term …

Although spatial variability in the distribution of soil organisms is often regarded as random,
recent attempts have found significant spatial structure at several scales. Understanding the …

Abstract The Last Glacial Termination led to major changes in ice sheet coverage that
disrupted global patterns of atmosphere and ocean circulation. Paleoclimate records from …