Integration of direct radiocarbon dating, genetic studies and taxonomy of small mammals to investigate the chronology of past climatic oscillations: The Last Glacial Maximum sequence of Grotta della Ferrovia (Fabriano, Italy)

• Published in: Quaternary Science Reviews
• Main Authors: Ceregatti, L., Berto, C., Fewlass, H., Baca, M., Luzi, E., Brancaleoni, G., Pereswiet-Soltan, A., Peresani, M.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2023
• Subjects: Southern Bank; Microtus arvalis
• Online Access: http://hdl.handle.net/21.11116/0000-000D-0E70-6

The recent developments in palaeoecological reconstruction methods, collagen extraction of small bone samples and ancient DNA analyses led us to test new approaches to enhance the chronological resolution of past climate reconstructions inferred from small mammal assemblages. Grotta della Ferrovia (Fabriano, Ancona, Italy, 40°25′36″N, 13°0′11″E, 215 m a.s.l.) is a small cave that opens on the southern bank of the Esino river, around 45 km west of Ancona. Discovered in 1966, it is famous among scholars because it is the first locality where the fossil birch mouse was recorded in Italy and because of the remarkable archaeological lithic evidence assemblage found in the cave related to the Late Epigravettian. Across the small mammal sequence, distributed into seven layers (from GDF7 to GDF2), two main phases can be recognized: in the first phase, from GDF7 to GDF5, Microtus arvalis is dominant over Microtus agrestis, in a poorly diversified assemblage. The sequence gradually changes in GDF4 and a second phase can be observed in GDF3 and GDF2, where Apodemus gr. sylvaticus-flavicollis dominates, but combined with a higher number of taxa. From GDF7 to GDF3, few individuals of Sicista cf. subtilis and Alexandromys oeconomus are recorded. Environmental and climatic reconstructions calculated with the Habitat Weighting and the Bioclimatic methods show a dominance of open meadows (GDF7 to GDF4) that were gradually replaced by closed or semi-closed forests (GDF3 and GDF2) in a context of gradually increasing temperature, shifting from a cold phase to conditions similar to the current ones in the area. Direct radiocarbon dates on 18 rodent bones and aDNA analyses on three Microtus arvalis teeth helped us to better understand the significance of the oscillation inferred from the small mammal sequences. A robust series of nine radiocarbon measurements from GDF7 to GDF5 shows that this part of the sequence accumulated between ∼24,600–19,600 cal BP (95.4% probability), which includes the final phases of the Last Glacial ...