|
|
Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/2883
|
| Authors: | Giaccio, B.* Isaia, R.* Fedele, F.* Di Canzio, E.* Hoffecker, J.* Ronchitelli, A.* Sinitsyn, A.* Anikovich, M.* Lisitsyn, S.* Popov, V.* |
| Title: | The Campanian Ignimbrite and Codola tephra layers: two temporal/stratigraphic markers for the Early Upper Palaeolithic in southern Italy and eastern Europe |
| Issue Date: | 19-Oct-2007 |
| DOI: | 10.1016/j.jvolgeores.2007.10.007 |
| Keywords: | Campanian ignimbrite Codola tephra layers |
| Abstract: | Tephra layers from archaeological sites in southern Italy and eastern Europe stratigraphically associated with
cultural levels containing Early Upper Palaeolithic industry were analysed. The results confirm the
occurrence of the Campanian Ignimbrite tephra (CI; c. 40 cal ka BP) at Castelcivita Cave (southern Italy),
Temnata Cave (Bulgaria) and in the Kostenki-Borshchevo area of the Russian Plain. This tephra, originated
from the largest eruption of the Phlegrean Field caldera, represents the widest volcanic deposit and one of the
most important temporal/stratigraphic markers of western Eurasia. At Paglicci Cave and lesser sites in the
Apulia region we recognise a chemically and texturally different tephra, which lithologically,
chronologically and chemically matches the physical and chemical characteristics of the Plinian eruption of
Codola; a poorly known Late Pleistocene explosive event from the Neapolitan volcanoes, likely Somma-
Vesuvius. For this latter, we propose a preliminary age estimate of c. 33 cal ka BP and a correlation to the
widespread C-10 marine tephra of the central Mediterranean. The stratigraphic position of both CI and
Codola tephra layers at Castelcivita and Paglicci help date the first and the last documented appearance of
Early Upper Palaeolithic industries of southern Italy to c. 41-40 and 33 cal ka BP, respectively, or between
two interstadial oscillations of the Monticchio pollen record – to which the CI and Codola tephras are
physically correlated – corresponding to the Greenland interstadials 10-9 and 5. In eastern Europe, the
stratigraphic and chronometric data seem to indicate an earlier appearance of the Early Upper Palaeolithic
industries, which would predate of two millennia at least the overlying CI tephra. The tephrostratigraphic
correlation indicates that in both regions the innovations connected with the so-called Early Upper
Palaeolithic – encompassing subsistence strategy and stone tool technology – appeared and evolved during
one of the most unstable climatic phases of the Last Glacial period. On this basis, the marked environmental
unpredictability characterising this time-span is seen as a potential ecological factor involved in the cultural
changes observed. |
| Appears in Collections: | Manuscripts 05.02.03. Volcanic eruptions 04.08.08. Volcanic risk 04.08.05. Volcanic rocks
|
Files in This Item:
| File |
Size | Format | Visibility |
| GiaIsaFed_2007.pdf | 2.27 MB | Adobe PDF | View/Open
|
| bozza IC- giaccio.pdf | 3.72 MB | Adobe PDF | View/Open
|
|
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.
|