Mediterranean tephrostratigraphy and peri-Tyrrhenian explosive activity revaluated in light of the 430-365 ka record from Fucino Basin (central Italy)

Autor: Monaco L.[1], Palladino D.M.[1], Gaeta M.[1], Marra F.[2], Sottili G.[1], Leicher N.[3], Mannella G.[4], Nomade S.[5], Pereira A.[6], Regattieri E.[7], Wagner B.[3], Zanchetta G.[2, 4, 12], Albert P.G.[8], Arienzo I.[9], D'Antonio M.[10], Petrosino P.[10], Manning C.J.[11], Giaccio B.[2

Publikováno v: Earth-Science Reviews
Earth-Science Reviews, Elsevier, 2021, 220, pp.103706. ⟨10.1016/j.earscirev.2021.103706⟩
Earth-Science Reviews, 2021, 220, pp.103706. ⟨10.1016/j.earscirev.2021.103706⟩
Earth-science reviews 220 (2021): 1–34. doi:10.1016/j.earscirev.2021.103706
info:cnr-pdr/source/autori:Monaco L.[1], Palladino D.M.[1], Gaeta M.[1], Marra F.[2], Sottili G.[1], Leicher N.[3], Mannella G.[4], Nomade S.[5], Pereira A.[6], Regattieri E.[7], Wagner B.[3], Zanchetta G.[2,4,12], Albert P.G.[8], Arienzo I.[9], D'Antonio M.[10], Petrosino P.[10], Manning C.J.[11], Giaccio B.[2,12]/titolo:Mediterranean tephrostratigraphy and peri-Tyrrhenian explosive activity revaluated in light of the 430-365 ka record from Fucino Basin (central Italy)/doi:10.1016%2Fj.earscirev.2021.103706/rivista:Earth-science reviews/anno:2021/pagina_da:1/pagina_a:34/intervallo_pagine:1–34/volume:220

International audience; Accurately reconstructing the scale and timing of dynamic processes, such as Middle-Late Pleistocene explosive volcanism and rapid climatic changes, requires rigorous and independent chronological constraints. In this framewor

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fbe17237d4299dee2a2e9286e857dc88
https://hal.archives-ouvertes.fr/hal-03265320