Discovery of cryptotephra at Middle–Upper Paleolithic sites Arma Veirana and Riparo Bombrini, Italy: a new link for broader geographic correlations
Autor: | Fabio Negrino, Eugene I. Smith, Guido S. Mariani, Julien Riel-Salvatore, Jamie Hodgkins, Jacob A. Harris, Racheal Johnsen, Jayde Hirniak, Caley M. Orr, David S. Strait, Claudine Gravel-Miguel, Marco Peresani, Curtis W. Marean, Shelby Fitch, Andrea Zerboni, Stefano Benazzi, Christopher E. Miller, Minghua Ren |
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Přispěvatelé: | Hirniak, Jayde N., Smith, Eugene I., Johnsen, Racheal, Ren, Minghua, Hodgkins, Jamie, Orr, Caley, Negrino, Fabio, Riel‐Salvatore, Julien, Fitch, Shelby, Miller, Christopher E., Zerboni, Andrea, Mariani, Guido S., Harris, Jacob A., Gravel‐Miguel, Claudine, Strait, David, Peresani, Marco, Benazzi, Stefano, Marean, Curtis W. |
Rok vydání: | 2019 |
Předmět: |
010506 paleontology
cryptotephra Middle Paleolithic radiocarbon dating tephrochronology Upper Paleolithic Middle Paleolithic Socio-culturale 010502 geochemistry & geophysics 01 natural sciences law.invention Middle Paleolithic Upper Paleolithic radiocarbon dating cryptotephra tephrochronology Arts and Humanities (miscellaneous) law Earth and Planetary Sciences (miscellaneous) Radiocarbon dating tephrochronology 0105 earth and related environmental sciences radiocarbon dating cryptotephra Upper Paleolithic Paleontology PE10_5 Archaeology 13. Climate action Tephrochronology Geology |
Zdroj: | Journal of Quaternary Science |
ISSN: | 1099-1417 0267-8179 |
DOI: | 10.1002/jqs.3158 |
Popis: | Chemical characterization of cryptotephra is critical for temporally linking archaeological sites. Here, we describe cryptotephra investigations of two Middle–Upper Paleolithic sites from north‐west Italy, Arma Veirana and Riparo Bombrini. Cryptotephra are present as small (75 wt.%) with low FeO ( 1 and P2 is also a high silica rhyolite (>75 wt.%) but with higher FeO (2.33–2.65 wt.%). Shards at Riparo Bombrini (P3) are of the same composition as P1 shards at Arma Veirana, providing a distinct link between deposits at both sites. Geochemical characteristics suggest three possible sources for P1 and P3: eruptions from Lipari Island (56–37.7 ka) in Italy, the Acigöl volcanic field (200–20 ka) in Turkey and the Miocene Kirka‐Phrigian caldera (18 Ma) in Turkey. Eruptions from Lipari Island are the most likely source for P1,3 cryptotephra. This study highlights how cryptotephra can benefit archaeology, by providing a direct link between Arma Veirana and Riparo Bombrini as well as other deposits throughout the Mediterranean. |
Databáze: | OpenAIRE |
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