During the glacial episodes of the Quaternary, European forests were restricted to small favourable spots, namely refugia, acting as biodiversity reservoirs. the Iberian, Italian and Balkan peninsulas have been considered as the main glacial refugia of trees in Europe. In this study, we estimate the composition of the last glacial forest in a coastal cave of the Cilento area (SW Italy) in seven time frames, spanning from the last Pleniglacial to the Late Glacial. Charcoal analyses were performed in seven archaeological layers. Furthermore, a paleoclimate modelling (Maxent) approach was used to complement the taxonomic identification of charcoal fragments to estimate the past potential distribution of tree species in Europe. Our results showed that the mesothermophilous forest survived in this region in the core of the Mediterranean basin during the Last Glacial Period (LGP, since ~36 ka cal BP), indicating that this area played an important role as a reservoir of woodland biodiversity. Here, Quercus pubescens was the most abundant component, followed by a wide variety of deciduous trees and Pinus nigra. Charcoal data also pointed at the crucial role of this coastal area, acting as a reservoir for warm temperate trees of genera Tilia, Carpinus and Sambucus, in LGP, in the Mediterranean region. Our modelling results showed that P. nigra might be the main candidate as a “Pinus sylvestris type” in the study site in the Last Glacial Maximum (LGM). Furthermore, we found that P. nigra might coexist with Q. pubescens in several European territories both currently and in the LGM. All models showed high levels of predictive performances. Our results highlight the advantage of combining different approaches such as charcoal analysis and ecological niche models to explore biogeographic questions about past and current forest distribution, with important implications to inform today’s forest management and conservation.

Charcoal analysis was carried out in two archaeological sites on the north slope of the Somma-Vesuvius volcano, not far from Naples. Both sites were inhabited between the 2nd century AD and AD 472, when a great Vesuvius eruption (so called Pollena eruption) buried them. In both sites, Castanea sativa wood was largely used for architectural structures as well as firewood. Ten ¹⁴C dates, spanning between the 1st and the 5th century AD, testify to a continuative use of this wood throughout the life of the sites. The comparison between archaeobotanical and pollen data from other sites in southern Italy suggests that chestnut woods were close to the sites studied and had a restricted spreading, possibly in a refugium area on Vesuvius' foothills. The match between archaeological charcoals and pollen data suggests that the Romans did not spread chestnut cultivation in the entire Campania region and that chestnut probably became a common timber in Campania starting from the 5th–6th century AD.