Revisiting the Y-3 tephrostratigraphic marker: a new diagnostic glass geochemistry, age estimate, and details on its climatostratigraphical context

Autor: Paul G. Albert a, b, Mark Hardiman c, d, Jörg Keller e, Emma L. Tomlinson f, a, Victoria C. Smith b, Anna J. Bourne c, g, Sabine Wulf h, Giovanni Zanchetta i, Roberto Sulpizio j, Ulrich C. Müller k, Jörg Pross k, l, Luisa Ottolinim, Ian P. Matthews c, Simon P.E. Blockley c, Martin A. Menzies a

Publikováno v: Quaternary science reviews 118 (2015): 105–121.
info:cnr-pdr/source/autori:Paul G. Albert a,b,*, Mark Hardiman c,d, Jörg Keller e, Emma L. Tomlinson f,a, Victoria C. Smith b, Anna J. Bourne c,g, Sabine Wulf h, Giovanni Zanchetta i, Roberto Sulpizio j, Ulrich C. Müller k, Jörg Pross k, l, Luisa Ottolinim, Ian P. Matthews c, Simon P.E. Blockley c, Martin A. Menzies a/titolo:Revisiting the Y-3 tephrostratigraphic marker: a new diagnostic glass geochemistry, age estimate, and details on its climatostratigraphical context/doi:/rivista:Quaternary science reviews/anno:2015/pagina_da:105/pagina_a:121/intervallo_pagine:105–121/volume:118

The 'Y-3' tephra is a crucial stratigraphic marker within the central Mediterranean region that falls close to the Marine Isotope Stage 3/2 transition and a cooling event proposed as a correlative of the North Atlantic Heinrich Stadial 3 (HS3). Conse

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