Fig 6. Climatostratigraphic position and age of the archaeological horizon inferred from the tephrostratigraphic correlation between Ficoncella and other successions containing the Sabatini Fall A pumice unit (~499 ka).

Mercure tephra record and ⁴⁰Ar/³⁹Ar ages of the proximal correlated units (AF-d; Fall A and Tufo Pisolitico di Trigoria, TPT) from ref. [86], and reference therein; Acerno tephra-pollen record and ⁴⁰Ar/³⁹Ar tephra ages from refs. [87–88]. The possible succession of the marine isotope stages (MIS), from MIS 14 to the MIS 12, is also shown.