The first glaciers at Ivrea, southern Alpine Foreland

Pleistocene Glaciations and their effects on Alpine topography have drawn scientific attention since well before the days of Penck and Brückner (1909), although this indomitable pair left a strong legacy to build upon. The onset of large-scale glaciations in the Alps relative to the growth of the other great Northern Hemisphere ice sheets remains a first-order question in the Quaternary sciences. Previous chronologies from the southern Alpine Foreland based on magnetostratigraphy (Muttoni et al. 2003) and from the northern Alpine Foreland based on 10Be-26Al burial dating (Knudsen et al. 2020) converge around 1.0–0.9 Ma, during the Middle Pleistocene Transition (~1.2–0.8 Ma). Extensive moraine complexes in the southern Alpine Foreland, such as those at Ivrea, offer a valuable opportunity to determine when glaciers advanced beyond the Alpine rangefront for the first time. The Ivrea Morainic Amphitheatre comprises interbedded glacial tills at the outlet of the Aosta Valley in NW Italy (Gianotti et al. 2015). The oldest tills have been attributed by previous workers to a stage before the Matuyama-Brunhes magnetic polarity reversal (~ 0.8 Ma). We apply 10Be-26Al burial dating to the oldest glacigenic deposits at Ivrea, utilizing the Monte Carlo-based inversion model, P-PINI (Particle-Pathway Inversion of Nuclide Inventories). Our preliminary results indicate that the first major glacial advance occurred ~ 1.3–1.1 Ma. We combine these analyses with detrital thermochronology measurements on pebbles collected from preglacial sediments at Ivrea. These pebbles indicate provenance from the Austroalpine Massifs and an absence of the External Massifs (Mont Blanc granites)-in contrast to the present-day Aosta Valley sediments, which show the cooling signature of the Mont Blanc granites. We reflect on the coincident timing of the exhumation of the External Massifs and the earliest large-scale Alpine glaciations at the onset of the Middle Pleistocene Transition.