TY - JOUR A1 - Leicher, Niklas A1 - Giaccio, Biagio A1 - Pereira, Alison A1 - Nomade, Sebastien A1 - Monaco, Lorenzo A1 - Mannella, Giorgio A1 - Galli, Paolo A1 - Peronance, Edoardo A1 - Palladino, Danilo Mauro A1 - Sottili, Gianluca A1 - Zanchetta, Giovanni A1 - Wagner, Bernd T1 - Central Mediterranean tephrochronology between 313 and 366 ka: New insights from the Fucino palaeolake sediment succession Y1 - 2022-12-09 VL - 52 IS - 2 SP - 240 EP - 271 JF - Boreas DO - 10.1111/bor.12610 PB - N2 - Thirty‐two tephra layers were identified in the time‐interval 313–366 ka (Marine Isotope Stages 9–10) of the Quaternary lacustrine succession of the Fucino Basin, central Italy. Twenty‐seven of these tephra layers yielded suitable geochemical material to explore their volcanic origins. Investigations also included the acquisition of geochemical data of some relevant, chronologically compatible proximal units from Italian volcanoes. The record contains tephra from some well‐known eruptions and eruptive sequences of Roman and Roccamonfina volcanoes, such as the Magliano Romano Plinian Fall, the Orvieto–Bagnoregio Ignimbrite, the Lower White Trachytic Tuff and the Brown Leucitic Tuff. In addition, the record documents eruptions currently undescribed in proximal (i.e. near‐vent) sections, suggesting a more complex history of the major eruptions of the Colli Albani, Sabatini, Vulsini and Roccamonfina volcanoes between 313 and 366 ka. Six of the investigated tephra layers were directly dated by single‐crystal‐fusion 40Ar/39Ar dating, providing the basis for a Bayesian age–depth model and a reassessment of the chronologies for both already known and dated eruptive units and for so far undated eruptions. The results provide a significant contribution for improving knowledge on the peri‐Tyrrhenian explosive activity as well as for extending the Mediterranean tephrostratigraphical framework, which was previously based on limited proximal and distal archives for that time interval. UR - http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/11249 ER -