http://www.cnr.it/ontology/cnr/individuo/prodotto/ID28463
The Y-3 tephra: A Last Glacial stratigraphic marker for the central Mediterranean basin (Articolo in rivista)
- Type
- Label
- The Y-3 tephra: A Last Glacial stratigraphic marker for the central Mediterranean basin (Articolo in rivista) (literal)
- Anno
- 2007-01-01T00:00:00+01:00 (literal)
- Alternative label
Zanchetta G., Sulpizio R., Giaccio B., Siani G., Paterne M., Wulf S., D'Orazio M. (2007)
The Y-3 tephra: A Last Glacial stratigraphic marker for the central Mediterranean basin
in Journal of volcanology and geothermal research
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Zanchetta G., Sulpizio R., Giaccio B., Siani G., Paterne M., Wulf S., D'Orazio M. (literal)
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
- doi:10.1016/j.jvolgeores.2007.08.017 (literal)
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- UniPisa, CNR IGG Pisa, UniBari, CNR IGAG, Orsayterre Universitè Paris XI, Laboratoire des Sciences du Climat et de l'Envirnment, CNRS-CEA Gif sur Yvette, University of Texas, (literal)
- Titolo
- The Y-3 tephra: A Last Glacial stratigraphic marker for the central Mediterranean basin (literal)
- Abstract
- The paper reviews the existing data on the Y-3 tephra layer, first recognised in the Ionian Sea (Mediterranean basin). The collection and collation of old and new data on distal tephra occurrences in terrestrial, marine and lacustrine successions indicate that the Y-3 layer is dispersed over a wide area of the central Mediterranean basin. The peculiar homogeneous chemical composition of this layer makes its recognition rather straightforward and permits it being distinguished from other stratigraphically adjacent tephras. The best age estimate for the Y-3 layer of ca 3031 cal ka BP, its peculiar stratigraphic position close to the Marine Isotope Stage 3/2 transition or Heinrich Event 3 onset, as well as its wide dispersion makes this layer an important marker to link and date late Pleistocene terrestrial and marine archives of the central mediterranean basin.
(literal)
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