There is a lack of high-resolution records of hydroclimate variability in the Eastern
Mediterranean from the late glacial and early Holocene. More knowledge of the speed of …

The Eastern Mediterranean, located at the meeting between the Mediterranean vegetation
of the Eurasian continent and the desert vegetation of the Saharan-Arabian desert belt, is …

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 …

Various types of abrupt/millennial-scale climate variability such as Dansgaard/Oeschger and
Heinrich Events characterized the last glacial period. Over the last decade, a number of …

We review palaeoenvironmental proxies and combinations of these relevant for
understanding hunter-gatherer niche construction activities in pre-agricultural Europe. Our …

Climate evolution of the Mediterranean region during the Holocene exhibits strong spatial
and temporal variability, which is notoriously difficult for models to reproduce. We propose …

The high-resolution multiproxy study of the Adriatic marine core MD 90-917 provides new
insights to reconstruct vegetation and regional climate changes over the southcentral …

Pollen assemblages of a sediment sequence (Co1215) from Lake Prespa reveal substantial
vegetational and environmental changes on a regional scale for the Lateglacial and …

This paper presents sedimentological, geochemical, and biological data from Lake Prespa
(Albania/Former Yugoslav Republic of Macedonia/Greece). The 320 cm core sequence …

Recurrent deposition of organic-rich sediment layers (sapropels) in the eastern
Mediterranean Sea is caused by complex interactions between climatic and biogeochemical …