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Tephrostratigraphy, chronology and climatic events of the Mediterranean basin during the Holocene

An overview

Bibliographic Data

ID12266542
AuthorsGiovanni Zanchetta (0000-0002-7080-9599, University of Pisa, INGV and IGG-GNR, Italy, corresponding author), Roberto Sulpizio (0000-0002-3930-5421, University of Bari Aldo Moro), Neil Roberts (0000-0001-5538-8653), Raffaello Cioni (0000-0002-2526-9095, University of Cagliari and INGV, Italy), Warren J Eastwood (0000-0002-6167-3829, University of Birmingham), Giuseppe Siani (0000-0002-2090-5320, CNRS-Université Paris-Sud XI, France), Benoît Caron (0000-0001-7051-4339, University of Pisa, Italy and CNRS-Université Paris-Sud XI, France), Martine Paterne (0000-0003-3715-6298, Laboratoire des Sciences du Climat et de l'Environment, France), Roberto Santacroce (University of Pisa)
Year2011
Volume21
Issue1
Pages33-52
Publication date2011-01-25
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683610377531
OpenAlexW2076081783
LanguageEN
Citations received41
References cited133

The identification and characterisation of high-frequency climatic changes during the Holocene requires natural archives with precise and accurate chronological control, which is usually difficult to achieve using only 14 C chronologies. The presence of time-spaced tephra beds in Quaternary Mediterranean successions represents an additional, independent tool for dating and correlating different sedimentary archives. These tephra layers are potentially useful for resolving long-standing issues in paleoclimatology and can help towards correlating terrestrial and marine paleoclimate archives. Known major tephras of regional extent derive from central and southern Italy, the Hellenic Arc, and from Anatolia. A striking feature of major Holocene tephra deposition events in the Mediterranean is that they are clustered rather than randomly distributed in time. Several tephra layers occurred at the time of the S1 sapropel formation between c. 8.4 and 9.0 ka BP (Mercato, Gabellotto-Fiumebianco/E1, Cappadocia) and other important tephra layers (Avellino, Agnano Monte Spina, ‘Khabur’ and Santorini/Thera) occurred during the second and third millennia BC, marking an important and complex phase of environmental changes during the mid- to late-Holocene climatic transition. There is great potential in using cryptotephra to overlap geographically Italian volcanic ashes with those originating from the Aegean and Anatolia, in order to connect regional tephrochronologies between the central and eastern Mediterranean

Archaeology · Chronology · Climate change · Geography · Holocene · Holocene climatic optimum · Mediterranean climate · Paleoclimatology · Physical geography · Quaternary · Sapropel · Sedimentary rock · Tephra · Tephrochronology · Volcano · Archaeology and ancient environmental studies · Geology and Paleoclimatology Research · Maritime and Coastal Archaeology · Geology · Oceanography · Paleontology

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Unique citing works41
Citations per year2,73
Citation span2011 - 2025 (15)
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