Eduardo di Marcantonio

Carbon isotope geochemistry of organic matter in volcanic paleosols constrains paleo‐environmental variations

The Fiorano quarry paleosol developed within the Colli Albani volcanic district (Italy) in the time interval bracketed by the deposition of the Pozzolanelle pyroclastic‐flow unit (365 ± 4 ka) and the emplacement of the Capo di Bove lava flow (277 ± 2 ka). The paleosol is characterized by an accretionary feature pro...